Sarmila/GeoWiki-Features huggingface dataset:
During the 3rd century BC, the Parthians migrated from the Central Asian steppe into northern Iran. Although subdued for a time by the Seleucids, they broke away in the 2nd century BC and established an independent state that steadily expanded at the expense of their former rulers, and through the course of the 2nd and early 1st centuries BC, they had conquered Persia, Mesopotamia, and Armenia.

Geographic entities mentioned:
surface_form: Persia
instance_of: Plateau
countries: Iran
coordinates: lat: 36.283333
lon: 59.05
However, the Iranian plateau never fell, as the Roman expeditions had always exhausted their offensive impetus by the time they reached lower Mesopotamia, and their extended line of communications through territory not sufficiently pacified exposed them to revolts and counterattacks. From the 4th century AD onwards, the Sasanians grew in strength and adopted the role of aggressor.

Geographic entities mentioned:
surface_form: Iranian plateau
instance_of: Plateau
countries: Iran
coordinates: lat: 36.283333
lon: 59.05
The Bürgenstock Funicular (; BB) is a funicular railway in the canton of Nidwalden, Switzerland. The line links the landing stage at Kehrsiten-Bürgenstock, served by the regular passenger boats of the Schifffahrtsgesellschaft des Vierwaldstättersees, with the Bürgenstock resort and its famous hotels. The funicular was opened in 1888 and was originally had an Abt rack braking rail.

Geographic entities mentioned:
surface_form: Bürgenstock
instance_of: Mountain
countries: Switzerland
coordinates: lat: 47.000305555556
lon: 8.3983888888889
Lake Kharkhari. gtj7tmf4453f8pfdg1jidh3sswq" xml:space="preserve">#REDIRECT Gabral Valley

Geographic entities mentioned:
surface_form: lake kharkhari
instance_of: Lake
countries: Pakistan
coordinates: lat: 35.6772
lon: 72.4015
In addition, the Vega de Antequera, watered by the river Guadalhorce, is a fertile agricultural area that provides cereals, olive oil, and vegetables in abundance. The nearby natural reserve of El Torcal, famous for its unstable limestone rocks, forms one of the most important karst landscapes in Europe.

Geographic entities mentioned:
surface_form: Vega de Antequera
instance_of: Valley
countries: Spain
coordinates: lat: 37.10694444
lon: -4.77111111
Across the Guadalhorce is &quot;Peña de los Enamorados&quot;, (&quot;The Lovers' Rock&quot;), named after the legend of two young Moorish lovers from rival clans who threw themselves from the rock while being pursued by the girl's father and his men.

Geographic entities mentioned:
surface_form: Peña de los Enamorados
instance_of: Mountain
countries: Spain
coordinates: lat: 37.06777778
lon: -4.49
Ogoki Lake. Ogoki Lake is a lake in Thunder Bay District, Ontario, Canada.

Geographic entities mentioned:
surface_form: ogoki lake
instance_of: Lake
countries: Canada
coordinates: lat: 50.83361111111111
lon: -87.17166666666667
As the southernmost suburb of the former Auckland City, it is considered part of South Auckland. The suburb's name is taken from the Māori-language name of the volcanic cone known as Mount Richmond. The name refers to &quot;the place of Tāhuhu&quot; — the eponymous ancestor, Tāhuhu-nui-a-Rangi, of Ngāi Tāhuhu. Demographics.

Geographic entities mentioned:
surface_form: Mount Richmond
instance_of: Mountain
countries: New Zealand
coordinates: lat: -36.9326
lon: 174.839
The vessel had previously been operated alongside her sister ship &quot;Grey Fox&quot; as part of Operation Lifespan in Northern Ireland since 1993 as LPV (Lough Patrol Vessel) &quot;Grey Wolf&quot; both vessels were based in their own special dock at Massereene barracks with access to 6 Mile Water in Lough Neagh, Northern Ireland where she was commanded and crewed by seven Royal Marines and two Royal Navy personnel conducting maritime counter terrorism, surveillance, intelligence and anti-smuggling operations.

Geographic entities mentioned:
surface_form: Lough Neagh
instance_of: Lake
countries: United Kingdom
coordinates: lat: 54.618333333333
lon: -6.3952777777778
Alkalihalobacillus lonarensis. &quot;Alkalihalobacillus lonarensis&quot; is a Gram-positive, alkalitolerant, endospore-forming, rod-shaped and motile bacterium from the genus &quot;Alkalihalobacillus&quot; which has been isolated from the Lonar Lake.

Geographic entities mentioned:
surface_form: Lonar Lake
instance_of: Lake
countries: India
coordinates: lat: 19.975
lon: 76.5075
The Soviet &quot;ekranoplan&quot; program continued with the support of Minister of Defence Dmitriy Ustinov. It produced the most successful &quot;ekranoplan&quot; so far, the 125-tonne A-90 &quot;Orlyonok&quot;. These craft were originally developed as high-speed military transports and were usually based on the shores of the Caspian Sea and Black Sea.

Geographic entities mentioned:
surface_form: Caspian Sea
instance_of: Body of water
Lake
countries: Iran
Russia
Kazakhstan
Azerbaijan
Turkmenistan
Russian Empire
Soviet Union
coordinates: lat: 42
lon: 50.5
Lake Tharthar raid. The Lake Tharthar raid was an Iraqi commando raid on a Secret Army of Islam training camp at Lake Tharthar on March 23, 2005. Background. The training camp, located in a remote region near Lake Tharthar, next to the Sunni Al Anbar and Salah ad Din provinces, was, according to Iraq officials, the largest guerrilla training camp discovered by that point in the war.

Geographic entities mentioned:
surface_form: Lake Tharthar
instance_of: Lake
countries: Iraq
coordinates: lat: 33.966666666667
lon: 43.183333333333
Background. The training camp, located in a remote region near Lake Tharthar, next to the Sunni Al Anbar and Salah ad Din provinces, was, according to Iraq officials, the largest guerrilla training camp discovered by that point in the war. The camp was shared by Ba’ath party loyalists and members of Al-Qaeda.

Geographic entities mentioned:
surface_form: Lake Tharthar
instance_of: Lake
countries: Iraq
coordinates: lat: 33.966666666667
lon: 43.183333333333
Bodfish, California. Bodfish is a census-designated place (CDP) in the southern Kern River Valley of the Southern Sierra Nevada, in Kern County, California, United States. Bodfish is located east-northeast of Bakersfield, at an elevation of. The population was 2,008 at the 2020 census, up from 1,956 at the 2010 census. History.

Geographic entities mentioned:
surface_form: Kern River Valley
instance_of: Valley
countries: United States
coordinates: lat: 35.6232
lon: -118.4845
Piani Palentini. The () is a plateau in upper Marsica, a subregion of Abruzzo, in central Italy. Description. The plains, located between a.s.l., are surrounded by mountain reliefs such as those of the Sirente-Velino group, Mount San Nicola, the Mount Bove massif (Carseolan Mountains), and the Mount Salviano range. Mounts Aurunzo and Girifalco separate the plains from the Nerfa Valley.

Geographic entities mentioned:
surface_form: Sirente
instance_of: Mountain
countries: Italy
coordinates: lat: 42.146111111111
lon: 13.611111111111
surface_form: Velino
instance_of: Mountain
countries: Italy
coordinates: lat: 42.15
lon: 13.366666666667
surface_form: mount salviano
instance_of: Mountain
countries: Italy
coordinates: lat: 42.031916666667
lon: 13.401222222222
Piani Palentini. The () is a plateau in upper Marsica, a subregion of Abruzzo, in central Italy. Description. The plains, located between a.s.l., are surrounded by mountain reliefs such as those of the Sirente-Velino group, Mount San Nicola, the Mount Bove massif (Carseolan Mountains), and the Mount Salviano range. Mounts Aurunzo and Girifalco separate the plains from the Nerfa Valley.

Geographic entities mentioned:
surface_form: piani palentini
instance_of: Valley
countries: Italy
coordinates: lat: 42.023194444444
lon: 13.375444444444
A few years after the first draining of lake Fucino through the building of the Tunnels of Claudius after 52 AD, the Piani Palentini were provided with an aqueduct to serve country villas and facilitate farming activities. Battle of Tagliacozzo.

Geographic entities mentioned:
surface_form: piani palentini
instance_of: Valley
countries: Italy
coordinates: lat: 42.023194444444
lon: 13.375444444444
The main quarry was on Turner's Hill, and in the 1960s was, in fact, two separate quarries, the Edwin Richards and Hailstone quarries, with a road between them leading to the top of the hill. At that time, hexagonal pillars similar to those of the Giant's Causeway in Northern Ireland could be seen on one of the quarry faces.

Geographic entities mentioned:
surface_form: Giant's Causeway
instance_of: Landform
countries: United Kingdom
coordinates: lat: 55.240833333333
lon: -6.5116666666667
The highway joins Fed. 15 and Fed. 80 in the southwest part of Guadalajara. For 148 km (92 mi), the Fed. 54 designation is substituted by Fed. 54D from Acatlán de Juárez, Jalisco to Ciudad Guzmán, a toll road. Across the southern Mexican Plateau, Fed. 54 connects Zacatecas in the southwest to Monterrey in the northeast at Fed. 57.

Geographic entities mentioned:
surface_form: Mexican Plateau
instance_of: Plateau
countries: Mexico
coordinates: lat: 24
lon: -103
Margarets Bay, Upper Tantallon and Lake Echo. Total cost of this deployment was projected to be $55 million. Although not listed, Fibe is currently being deployed in the Fall River area, as of early November 2011. The service expanded to the Annapolis Valley in early 2022. In May 2023, Citywide Communications and Purple Cow began using Bell Aliant TV Following Eastlink’s loss of Corus channels.

Geographic entities mentioned:
surface_form: Annapolis Valley
instance_of: Valley
countries: Canada
coordinates: lat: 44.979166666666664
lon: -64.89222222222222
A minority of scholars have argued that Gregory affirmed only the universal resurrection. In the &quot;Life of Moses&quot;, Gregory writes that just as the darkness left the Egyptians after three days, perhaps redemption [ἀποκατάστασις] will be extended to those suffering in hell [γέεννα].

Geographic entities mentioned:
surface_form: γέεννα
instance_of: Valley
countries: Israel
coordinates: lat: 31.76916667
lon: 35.22805556
In the three years (1957–60) during which the &quot;regroupement&quot; program was followed, more than 2 million Algerians were removed from their villages, mostly in the mountainous areas, and resettled in the plains, where it was difficult to reestablish their previous economic and social systems. Living conditions in the fortified villages were poor.

Geographic entities mentioned:
surface_form: mountainous areas
instance_of: Mountain
countries: Algeria
France
coordinates: lat: 36.607807
lon: 3.4443945
Gildersleeve Mountain is located in the Chapin Forest Reservation of Lake Metroparks and is referred to as the &quot;scenic overlook&quot;. Geography. The summit of Gildersleeve Mountain is above sea level. above Lake Erie. The shoreline of Lake Erie is approximately north west of the summit. Gildersleeve Mountain marks the beginning of the Allegheny Plateau in the area.

Geographic entities mentioned:
surface_form: Lake Erie
instance_of: Lake
countries: Canada
United States
coordinates: lat: 42.25
lon: -80.99972222222222
Gildersleeve Mountain. Gildersleeve Mountain is a summit located in Kirtland, Ohio, United States. Gildersleeve Mountain is interesting and important because it is within one of the largest and most densely populated metropolitan areas in the United States (regional population 2.9 million). It is a relatively unspoiled and unique area just from downtown Cleveland.

Geographic entities mentioned:
surface_form: cleveland
instance_of: Mountain
countries: United States
coordinates: lat: 52.822222222222
lon: -169.945
The southern side of the feature has a much less dramatic transition, falling only to the surrounding highlands. Gildersleeve Mountain is one of the more obvious geographic features of the Cleveland region. It is visible when the view is unobstructed by buildings or trees from downtown Cleveland, Mayfield Heights, and from the shore and waters of Lake Erie.

Geographic entities mentioned:
surface_form: cleveland
instance_of: Mountain
countries: United States
coordinates: lat: 52.822222222222
lon: -169.945
Gildersleeve Mountain is one of the more obvious geographic features of the Cleveland region. It is visible when the view is unobstructed by buildings or trees from downtown Cleveland, Mayfield Heights, and from the shore and waters of Lake Erie. It is obvious when looking to the south from the lake or northeast from any tall building near the lake shore in Cuyahoga County.

Geographic entities mentioned:
surface_form: cleveland
instance_of: Mountain
countries: United States
coordinates: lat: 52.822222222222
lon: -169.945
Gildersleeve Mountain also has views of Lake Erie from locations near the summit. From one location the view to the west and southwest affords a view of the downtown Cleveland skyline, away. On clear days the stacks in Lorain or Avon Lake may be visible, and on exceptional days the plume from cooling towers at the Davis-Besse, or Permian, nuclear power stations may be visible far to the west.

Geographic entities mentioned:
surface_form: cleveland
instance_of: Mountain
countries: United States
coordinates: lat: 52.822222222222
lon: -169.945
Another feature of interest is a cabin foundation on the northern end of the summit. There was a chimney associated with this foundation until it was blown down during the Ohio Fireworks Derecho that struck the Cleveland region on July 4, 1969. This storm also toppled several hundred trees on Gildersleeve Mountain.

Geographic entities mentioned:
surface_form: cleveland
instance_of: Mountain
countries: United States
coordinates: lat: 52.822222222222
lon: -169.945
These creeks are augmented by rain and snow melt. They create ravine systems that cut through layers of rock and provide interesting places to study local geology. The Quarry Creek ravine accessible from the Old South Church property cuts down to the Cleveland Shale layer before crossing Eagle road. Geology.

Geographic entities mentioned:
surface_form: cleveland
instance_of: Mountain
countries: United States
coordinates: lat: 52.822222222222
lon: -169.945
Named for the Chagrin River and easily found in the river valley, Chagrin shale is blue-gray in color, an offshore alluvial, silt shale of the Devonian period. This layer is found below about msl and is found when drilling wells on the slopes of Gildersleeve Mountain. The next layer is Cleveland shale. This is a black shale that is an important source of local fossils.

Geographic entities mentioned:
surface_form: cleveland
instance_of: Mountain
countries: United States
coordinates: lat: 52.822222222222
lon: -169.945
This is a black shale that is an important source of local fossils. Again Cleveland shale is not visible on Gildersleeve Mountain but can easily be found in the nearby Chagrin River valley between 800 and msl. Bedford shale is found above the Cleveland Shale layer. This material marks the uncertain transition between the Devonian and Pennsylvanian periods in the region.

Geographic entities mentioned:
surface_form: cleveland
instance_of: Mountain
countries: United States
coordinates: lat: 52.822222222222
lon: -169.945
Hermit thrush is a probable nesting species. Black-throated green warbler nests in the ledges and hemlock hardwood forest. Purple finch is an occasional nester. Dark-eyed junco, is a prolific nester and abundant year round on Gildersleeve mountain, not just in the winter, as in most of the Cleveland region. Pine siskin is another very rare nesting species first verified in 2009.

Geographic entities mentioned:
surface_form: cleveland
instance_of: Mountain
countries: United States
coordinates: lat: 52.822222222222
lon: -169.945
surface_form: gildersleeve mountain
instance_of: Mountain
countries: United States
coordinates: lat: 41.594166666667
lon: -81.359166666667
From one location the view to the west and southwest affords a view of the downtown Cleveland skyline, away. On clear days the stacks in Lorain or Avon Lake may be visible, and on exceptional days the plume from cooling towers at the Davis-Besse, or Permian, nuclear power stations may be visible far to the west. Point Rondeau, Ontario, away, is the closest point on the Canadian shore of Lake Erie.

Geographic entities mentioned:
surface_form: lake may
instance_of: Lake
countries: United States
coordinates: lat: 47.09055556
lon: -94.59333333
Point Rondeau, Ontario, away, is the closest point on the Canadian shore of Lake Erie. However, the distance to the horizon at the lookout is only, so while the Canadian waters of Lake Erie are visible from Gildersleeve Mountain, the Canadian shore is not. On clear nights, lights are visible on the horizon to the northwest but it is uncertain if these are on the Canadian shore.

Geographic entities mentioned:
surface_form: the lookout
instance_of: Mountain
countries: United States
coordinates: lat: 40.509444444444
lon: -75.346111111111
surface_form: gildersleeve mountain
instance_of: Mountain
countries: United States
coordinates: lat: 41.594166666667
lon: -81.359166666667
It is a relatively unspoiled and unique area just from downtown Cleveland. While this is not unique in a region where urban and suburban forest preserves abound, it is one of only two natural areas with higher elevations and unique rock outcroppings. Little Mountain, which is near the Holden Arboretum, is similar to Gildersleeve Mountain but is accessible on guided walks only.

Geographic entities mentioned:
surface_form: little mountain
instance_of: Mountain
countries: United States
coordinates: lat: 34.186944444444
lon: -81.413611111111
surface_form: little mountain
instance_of: Mountain
countries: United States
coordinates: lat: 35.57
lon: -85.2808
surface_form: gildersleeve mountain
instance_of: Mountain
countries: United States
coordinates: lat: 41.594166666667
lon: -81.359166666667
Flora. Prior to European settlement the area was a vast northern hardwood forest. On Gildersleeve mountain this probably consisted of 3 types of forest. Beech-maple forest, hemlock hardwood forest, and oak hickory forest. as remnant stands of all three types remain. Old growth oak and maple can be found in a few locations where they were not claimed by 19th-century logging.

Geographic entities mentioned:
surface_form: hemlock
instance_of: Lake
countries: United States
coordinates: lat: 42.718611111111
lon: -77.608888888889
Blue-headed vireo, is found in the ledges and hemlocks. Hermit thrush is a probable nesting species. Black-throated green warbler nests in the ledges and hemlock hardwood forest. Purple finch is an occasional nester. Dark-eyed junco, is a prolific nester and abundant year round on Gildersleeve mountain, not just in the winter, as in most of the Cleveland region.

Geographic entities mentioned:
surface_form: hemlock
instance_of: Lake
countries: United States
coordinates: lat: 42.718611111111
lon: -77.608888888889
This storm also toppled several hundred trees on Gildersleeve Mountain. The foundation is now in an overgrown area of what used to be the Panorama Point picnic area. Although signage still calls out this area, the panoramic view from this location is no longer viable because trees have been allowed to grow and obscure the view.

Geographic entities mentioned:
surface_form: panorama point
instance_of: Mountain
countries: United States
coordinates: lat: 41.0105
lon: -104.03
Also of interest are the remnants of a cistern at the base of an outcropping to the west of the cabin foundation. These may be found by following the base of the rock outcroppings to the west of the Panorama Point area. The water caught by this cistern is filtered through the Sharon conglomerate and seeps out of the base of the outcropping.

Geographic entities mentioned:
surface_form: panorama point
instance_of: Mountain
countries: United States
coordinates: lat: 41.0105
lon: -104.03
The geology of the area reflects this transition. The lowest visible bedrock is Chagrin Shale. Named for the Chagrin River and easily found in the river valley, Chagrin shale is blue-gray in color, an offshore alluvial, silt shale of the Devonian period. This layer is found below about msl and is found when drilling wells on the slopes of Gildersleeve Mountain. The next layer is Cleveland shale.

Geographic entities mentioned:
surface_form: river valley
instance_of: Valley
countries: United States
coordinates: lat: 35.36
lon: -93.37
The next layer is Cleveland shale. This is a black shale that is an important source of local fossils. Again Cleveland shale is not visible on Gildersleeve Mountain but can easily be found in the nearby Chagrin River valley between 800 and msl. Bedford shale is found above the Cleveland Shale layer.

Geographic entities mentioned:
surface_form: river valley
instance_of: Valley
countries: United States
coordinates: lat: 35.36
lon: -93.37
surface_form: gildersleeve mountain
instance_of: Mountain
countries: United States
coordinates: lat: 41.594166666667
lon: -81.359166666667
Gildersleeve Mountain. Gildersleeve Mountain is a summit located in Kirtland, Ohio, United States. Gildersleeve Mountain is interesting and important because it is within one of the largest and most densely populated metropolitan areas in the United States (regional population 2.9 million). It is a relatively unspoiled and unique area just from downtown Cleveland.

Geographic entities mentioned:
surface_form: gildersleeve mountain
instance_of: Mountain
countries: United States
coordinates: lat: 41.594166666667
lon: -81.359166666667
Little Mountain, which is near the Holden Arboretum, is similar to Gildersleeve Mountain but is accessible on guided walks only. Gildersleeve Mountain is located in the Chapin Forest Reservation of Lake Metroparks and is referred to as the &quot;scenic overlook&quot;. Geography. The summit of Gildersleeve Mountain is above sea level. above Lake Erie.

Geographic entities mentioned:
surface_form: gildersleeve mountain
instance_of: Mountain
countries: United States
coordinates: lat: 41.594166666667
lon: -81.359166666667
Gildersleeve Mountain is located in the Chapin Forest Reservation of Lake Metroparks and is referred to as the &quot;scenic overlook&quot;. Geography. The summit of Gildersleeve Mountain is above sea level. above Lake Erie. The shoreline of Lake Erie is approximately north west of the summit. Gildersleeve Mountain marks the beginning of the Allegheny Plateau in the area.

Geographic entities mentioned:
surface_form: gildersleeve mountain
instance_of: Mountain
countries: United States
coordinates: lat: 41.594166666667
lon: -81.359166666667
About 60% of Gildersleeve Mountain is within the Chapin Forest Reservation, which was acquired by the state of Ohio in 1949 and has been managed by the Lake County Metropolitan Park District since 1966, located along State Route 306/Chillicothe Road.

Geographic entities mentioned:
surface_form: gildersleeve mountain
instance_of: Mountain
countries: United States
coordinates: lat: 41.594166666667
lon: -81.359166666667
Trails that may be used for hiking, bicycling, horseback riding, and cross country skiing in winter cross the public lands and circle the summit. Over 50 private residences are on the slopes of Gildersleeve Mountain. An active natural gas well was drilled in 2006, and the forested areas are logged for hardwood maple and oak.

Geographic entities mentioned:
surface_form: gildersleeve mountain
instance_of: Mountain
countries: United States
coordinates: lat: 41.594166666667
lon: -81.359166666667
Commercial exploitation of these resources ceased in 1968. Topology. As the map to the right shows, the topography of Gildersleeve Mountain had been changed significantly by human activity. The sand and gravel quarry on the west side was active for more than 100 years before shutting down in 1968 and being acquired by the state of Ohio.

Geographic entities mentioned:
surface_form: gildersleeve mountain
instance_of: Mountain
countries: United States
coordinates: lat: 41.594166666667
lon: -81.359166666667
Development, although not shown on the map, also changed the topography. Some of the cleared areas and some of the forested areas are subdivided and have light duty roads with private homes. This is mostly on the southeast side of Gildersleeve Mountain. In 2007 the former quarry access area and orchard on the west side will be developed into home sites.

Geographic entities mentioned:
surface_form: gildersleeve mountain
instance_of: Mountain
countries: United States
coordinates: lat: 41.594166666667
lon: -81.359166666667
There was a chimney associated with this foundation until it was blown down during the Ohio Fireworks Derecho that struck the Cleveland region on July 4, 1969. This storm also toppled several hundred trees on Gildersleeve Mountain. The foundation is now in an overgrown area of what used to be the Panorama Point picnic area.

Geographic entities mentioned:
surface_form: gildersleeve mountain
instance_of: Mountain
countries: United States
coordinates: lat: 41.594166666667
lon: -81.359166666667
The water caught by this cistern is filtered through the Sharon conglomerate and seeps out of the base of the outcropping. There are numerous seeps all around Gildersleeve Mountain, and they are the source of the creeks that run off into the Chagrin River watershed. These creeks are augmented by rain and snow melt.

Geographic entities mentioned:
surface_form: gildersleeve mountain
instance_of: Mountain
countries: United States
coordinates: lat: 41.594166666667
lon: -81.359166666667
The geology of the area reflects this transition. The lowest visible bedrock is Chagrin Shale. Named for the Chagrin River and easily found in the river valley, Chagrin shale is blue-gray in color, an offshore alluvial, silt shale of the Devonian period. This layer is found below about msl and is found when drilling wells on the slopes of Gildersleeve Mountain. The next layer is Cleveland shale.

Geographic entities mentioned:
surface_form: gildersleeve mountain
instance_of: Mountain
countries: United States
coordinates: lat: 41.594166666667
lon: -81.359166666667
Bedford shale is found above the Cleveland Shale layer. This material marks the uncertain transition between the Devonian and Pennsylvanian periods in the region. This layer is found in the ravines that run off the slopes of Gildersleeve Mountain. Bedford shale is a sand shale and is characterized by its roughly 90° cleavage pattern.

Geographic entities mentioned:
surface_form: gildersleeve mountain
instance_of: Mountain
countries: United States
coordinates: lat: 41.594166666667
lon: -81.359166666667
Berea sandstone is found from around msl to roughly msl. However, at this point it should be mentioned that the rock structure around Gildersleeve Mountain is by no means uniform. Millions of years of glaciation and resulting erosion and fill have resulted in many ravines that have been subsequently filled with glacial till and alluvial clays.

Geographic entities mentioned:
surface_form: gildersleeve mountain
instance_of: Mountain
countries: United States
coordinates: lat: 41.594166666667
lon: -81.359166666667
Millions of years of glaciation and resulting erosion and fill have resulted in many ravines that have been subsequently filled with glacial till and alluvial clays. Still, Berea sandstone is found in outcroppings and in other areas on Gildersleeve Mountain. In the nineteenth century it was quarried from the Stannard Quarry, what is now Quarry Pond, near Chillicothe Road.

Geographic entities mentioned:
surface_form: gildersleeve mountain
instance_of: Mountain
countries: United States
coordinates: lat: 41.594166666667
lon: -81.359166666667
Berea sandstone is still used as a local building material. Sharon conglomerate is found beginning around msl. It is the predominant outcropping on Gildersleeve Mountain. Sharon Conglomerate is a sandstone imbedded with white quartz pebbles. It is hypothesized this rock was created by fast-running streams, running down ancient mountains.

Geographic entities mentioned:
surface_form: gildersleeve mountain
instance_of: Mountain
countries: United States
coordinates: lat: 41.594166666667
lon: -81.359166666667
Faster-running water carried larger pebbles along with the sand, and this was deposited very near shore, or in river or stream deltas and estuaries. It is Sharon conglomerate outcroppings that up make most of the spectacular ledges that are found on the southeast, north, and western sides of Gildersleeve Mountain.

Geographic entities mentioned:
surface_form: gildersleeve mountain
instance_of: Mountain
countries: United States
coordinates: lat: 41.594166666667
lon: -81.359166666667
In some areas, there are vertical faces of over with very steep slopes at the base. In these areas the elevation change is dramatic, going from to in under of horizontal distance. As mentioned earlier, glaciation has played an important part in the geology of Gildersleeve Mountain. During the Wisconsin glaciation, ice sheets more than a mile thick covered the region.

Geographic entities mentioned:
surface_form: gildersleeve mountain
instance_of: Mountain
countries: United States
coordinates: lat: 41.594166666667
lon: -81.359166666667
Glaciers are the major erosive force in the region and ground down the higher elevations while scooping out the [Great Lakes]. The hard Sharon conglomerate is more resistant to this grinding action. Glacial ice is not the only erosive force to act upon Gildersleeve Mountain. Glacial melt released huge amounts of water that flooded the landscape.

Geographic entities mentioned:
surface_form: gildersleeve mountain
instance_of: Mountain
countries: United States
coordinates: lat: 41.594166666667
lon: -81.359166666667
A rare species of grass may be found in the ledges. Unfortunately, deer browse has seriously reduced the abundance of herbaceous species. The outcroppings have additional interest because club mosses and lichens can be found on their surfaces. Interesting fungi are present, but these disappear quickly given the fact that Gildersleeve Mountain is within a major American metropolitan area. Fauna.

Geographic entities mentioned:
surface_form: gildersleeve mountain
instance_of: Mountain
countries: United States
coordinates: lat: 41.594166666667
lon: -81.359166666667
Fauna. The seeps and creeks running along the slopes provide a unique habitat. Dragonflies and damselflies (&quot;odonata&quot;) are of special interest to naturalists of the region and Gildersleeve mountain has been a site of recent discoveries. The first tiger spiketail, documented in Ohio, was discovered on Gildersleeve Mountain, in 2004.

Geographic entities mentioned:
surface_form: gildersleeve mountain
instance_of: Mountain
countries: United States
coordinates: lat: 41.594166666667
lon: -81.359166666667
The first tiger spiketail, documented in Ohio, was discovered on Gildersleeve Mountain, in 2004. Other rare dragonflies documented on Gildersleeve Mountain include gray petaltail, comet darner, ocellated darner, and twin spotted spiketail. Crayfish are found in the creeks.

Geographic entities mentioned:
surface_form: gildersleeve mountain
instance_of: Mountain
countries: United States
coordinates: lat: 41.594166666667
lon: -81.359166666667
Black rat snakes, and garter snakes are common. One of Kirtland's first settlers, Christopher Crary, recalled rattlesnakes in the 1820s or 30s in his memoir: &quot;On Gildersleeve mountain twenty three were killed in one day, and they soon became extinct.&quot; These were probably eastern timber rattlesnake. American toads are found along with spring peepers and gray tree frogs.

Geographic entities mentioned:
surface_form: gildersleeve mountain
instance_of: Mountain
countries: United States
coordinates: lat: 41.594166666667
lon: -81.359166666667
American toads are found along with spring peepers and gray tree frogs. Pickerel frogs are found in the creeks. Green frogs are found in the vernal pools and other water. Bullfrogs are found in the ponds on the northwestern slope
Many species of birds can be found on Gildersleeve mountain. Barred owls are common year round residents and can be found by listening and watching carefully.

Geographic entities mentioned:
surface_form: gildersleeve mountain
instance_of: Mountain
countries: United States
coordinates: lat: 41.594166666667
lon: -81.359166666667
Dark-eyed junco, is a prolific nester and abundant year round on Gildersleeve mountain, not just in the winter, as in most of the Cleveland region. Pine siskin is another very rare nesting species first verified in 2009. Interesting and very rare migrant species have been found on or seen from Gildersleeve mountain. Tundra swans are expected in fall as they fly over on their way south.

Geographic entities mentioned:
surface_form: gildersleeve mountain
instance_of: Mountain
countries: United States
coordinates: lat: 41.594166666667
lon: -81.359166666667
White tailed deer are common. Red fox have declined as coyote have increased in numbers. Evidence of bobcat has been found but confirmation of this species will require a specimen. In June 2004, a black bear made yet another contemporary appearance on Gildersleeve mountain. This time leaving tracks, tearing up a trash receptacles. History.

Geographic entities mentioned:
surface_form: gildersleeve mountain
instance_of: Mountain
countries: United States
coordinates: lat: 41.594166666667
lon: -81.359166666667
Writer Elizabeth F. Ellet was a native of the town. Geography. Sodus Point is located at (43.269332, -76.987608). According to the United States Census Bureau, the village has a total area of, of which is land and 0.67% is water. The village is on the shore of Lake Ontario on a point of land on the northwest edge of Sodus Bay, an arm of Lake Ontario.

Geographic entities mentioned:
surface_form: Lake Ontario
instance_of: Lake
countries: Canada
United States
coordinates: lat: 43.72888888888889
lon: -78.10638888888889
History. The church was located along the ancient road that linked the Lunigiana valley near Lucca with the Po valley; this church was documented by 979, under the pieve of Diecimo. It operated an adjacent hostel for pilgrims. The present church, visible from the banks of the Serchio, was built in the 12th century.

Geographic entities mentioned:
surface_form: Po valley
instance_of: Valley
countries: Italy
coordinates: lat: 45.330277777778
lon: 9.7988888888889
Anderson Lake (Nova Scotia). Anderson Lake is a lake of Halifax Regional Municipality, Nova Scotia, Canada.

Geographic entities mentioned:
surface_form: anderson lake
instance_of: Lake
countries: Canada
coordinates: lat: 44.73441
lon: -63.86179
surface_form: anderson lake (nova scotia)
instance_of: Lake
countries: Canada
coordinates: lat: 44.7266
lon: -63.6197
surface_form: anderson lake
instance_of: Lake
countries: Canada
coordinates: lat: 49.73
lon: -125.19861
surface_form: anderson lake
instance_of: Lake
countries: Canada
coordinates: lat: 51.03333
lon: -102.15047
surface_form: anderson lake
instance_of: Lake
countries: Canada
coordinates: lat: 50.6333
lon: -122.417
Anderson Lake (Nova Scotia). Anderson Lake is a lake of Halifax Regional Municipality, Nova Scotia, Canada.

Geographic entities mentioned:
surface_form: anderson lake
instance_of: Lake
countries: Canada
coordinates: lat: 44.73441
lon: -63.86179
surface_form: anderson lake
instance_of: Lake
countries: Canada
coordinates: lat: 44.7266
lon: -63.6197
surface_form: anderson lake
instance_of: Lake
countries: Canada
coordinates: lat: 49.73
lon: -125.19861
surface_form: anderson lake
instance_of: Lake
countries: Canada
coordinates: lat: 51.03333
lon: -102.15047
surface_form: anderson lake
instance_of: Lake
countries: Canada
coordinates: lat: 50.6333
lon: -122.417
Kashmiri Muslims. Kashmiri Muslims are ethnic Kashmiris who practice Islam and are native to the Kashmir Valley of Indian-administered Jammu and Kashmir. The majority of Kashmiri Muslims are Sunni, while Shias form a minority. They refer to themselves as &quot;Koshur&quot; in the Kashmiri language. Presently, the Kashmiri Muslim population is predominantly found in Kashmir Valley.

Geographic entities mentioned:
surface_form: Kashmir Valley
instance_of: Valley
countries: India
coordinates: lat: 34.0333
lon: 74.6667
In the Jammu region, sizeable population of Kashmiri Muslims lives in the Doda, Ramban and Kishtwar districts, sometimes collectively referred to as the Chenab valley. There are also ethnic Kashmiri Muslim populations inhabiting Neelum and Leepa Valleys of Pakistani-administrated Kashmir. Since 1947, many ethnic Kashmiri Muslims have also lived in Punjab, Pakistan.

Geographic entities mentioned:
surface_form: Leepa Valley
instance_of: Valley
countries: Pakistan
coordinates: lat: 34.3136
lon: 73.8981
There are also ethnic Kashmiri Muslim populations inhabiting Neelum and Leepa Valleys of Pakistani-administrated Kashmir. Since 1947, many ethnic Kashmiri Muslims have also lived in Punjab, Pakistan. Many ethnic Kashmiri Muslims from the Kashmir Valley also migrated to the Punjab region during Dogra and Sikh rule. The Kashmiri language is the mother tongue of majority of Kashmiri Muslims. History.

Geographic entities mentioned:
surface_form: Kashmir Valley
instance_of: Valley
countries: India
coordinates: lat: 34.0333
lon: 74.6667
Dogra Regime. The 100 year Dogra regime turned out to be a disaster for the Muslim peasantry of Kashmir Valley. Walter Lawrence described the conditions of the Kashmir Valley's peasantry as being 'desperate' and noted that the valley's peasantry attributed their miseries to the Maharajah's deputies rather than the rulers themselves.

Geographic entities mentioned:
surface_form: Kashmir Valley
instance_of: Valley
countries: India
coordinates: lat: 34.0333
lon: 74.6667
Another notable member of the Kashmiri Muslim diaspora in Punjab was Muhammad Iqbal (who took pride in his Brahman ancestry and whose poetry displayed a keen sense of belonging to the Kashmir Valley). Another famous proud Kashmiri writer from Punjab was Saadat Hasan Manto. According to the 1921 Census the total Kashmiri population in Punjab was 169,761.

Geographic entities mentioned:
surface_form: Kashmir Valley
instance_of: Valley
countries: India
coordinates: lat: 34.0333
lon: 74.6667
Kashmiris settled for generations in the Punjab were unable to own land, including the family of Muhammad Iqbal. Scholar Chitralekha Zutshi states that Kashmiri Muslims settled in the Punjab retained emotional and familial links to Kashmir and felt obliged to struggle for the freedom of their brethren in the Valley.

Geographic entities mentioned:
surface_form: Valley
instance_of: Valley
countries: India
coordinates: lat: 34.0333
lon: 74.6667
It lies in the La Paz Department, Murillo Province, Palca Municipality. Ch'iyar Qullu is situated near the river Chuqi Quta (&quot;gold lake&quot;, &quot;Choquekkota&quot;), south-west of the lake Ch'uxña Quta and north-west of the village of Chuqi Quta &quot;(Choquecota, Choquekhota)&quot;.

Geographic entities mentioned:
surface_form: ch'uxña quta
instance_of: Mountain
countries: Bolivia
coordinates: lat: -15.7425
lon: -68.5806
surface_form: ch'uxña quta
instance_of: Lake
countries: Bolivia
coordinates: lat: -15.12861111
lon: -69.15333333
surface_form: ch'uxña quta
instance_of: Lake
countries: Bolivia
coordinates: lat: -16.48611111111111
lon: -67.92916666666666
surface_form: ch'uxña quta
instance_of: Lake
countries: Bolivia
coordinates: lat: -15.014166666666666
lon: -69.09083333333334
surface_form: ch'uxña quta
instance_of: Mountain
countries: Bolivia
coordinates: lat: -17.8775
lon: -68.9731
Tata Ch'iyar Qullu. Tata Ch'iyar Qullu (Aymara &quot;tata&quot; father, lord, sir, &quot;ch'iyara&quot; black, &quot;qullu&quot; mountain, &quot;Father Black Mountain&quot;, also spelled &quot;Tata Chiar Khollu&quot;) or just Ch'iyar Qullu &quot;(Charkkollu)&quot; is a mountain in the Bolivian Andes, about high. It lies in the La Paz Department, Murillo Province, Palca Municipality.

Geographic entities mentioned:
surface_form: ch'iyar qullu
instance_of: Mountain
countries: Bolivia
coordinates: lat: -15.8583
lon: -68.5819
surface_form: ch'iyar qullu
instance_of: Mountain
countries: Bolivia
coordinates: lat: -16.4636
lon: -67.9556
surface_form: ch'iyar qullu
instance_of: Mountain
countries: Bolivia
coordinates: lat: -16.6144
lon: -67.81
surface_form: ch'iyar qullu
instance_of: Mountain
countries: Bolivia
coordinates: lat: -19.43333333
lon: -67.38333333
surface_form: ch'iyar qullu
instance_of: Mountain
countries: Bolivia
coordinates: lat: -16.5044
lon: -67.975
surface_form: ch'iyar qullu
instance_of: Mountain
countries: Bolivia
coordinates: lat: -16.2556
lon: -68.2831
surface_form: tata ch'iyar qullu
instance_of: Mountain
countries: Bolivia
coordinates: lat: -16.50222222
lon: -67.94166667
Tata Ch'iyar Qullu. Tata Ch'iyar Qullu (Aymara &quot;tata&quot; father, lord, sir, &quot;ch'iyara&quot; black, &quot;qullu&quot; mountain, &quot;Father Black Mountain&quot;, also spelled &quot;Tata Chiar Khollu&quot;) or just Ch'iyar Qullu &quot;(Charkkollu)&quot; is a mountain in the Bolivian Andes, about high. It lies in the La Paz Department, Murillo Province, Palca Municipality.

Geographic entities mentioned:
surface_form: ch'iyar qullu
instance_of: Mountain
countries: Bolivia
coordinates: lat: -15.8583
lon: -68.5819
surface_form: ch'iyar qullu
instance_of: Mountain
countries: Bolivia
coordinates: lat: -15.8583
lon: -68.5819
surface_form: ch'iyar qullu
instance_of: Mountain
countries: Bolivia
coordinates: lat: -16.4636
lon: -67.9556
surface_form: ch'iyar qullu
instance_of: Mountain
countries: Bolivia
coordinates: lat: -16.4636
lon: -67.9556
surface_form: ch'iyar qullu
instance_of: Mountain
countries: Bolivia
coordinates: lat: -16.6144
lon: -67.81
surface_form: ch'iyar qullu
instance_of: Mountain
countries: Bolivia
coordinates: lat: -16.6144
lon: -67.81
surface_form: ch'iyar qullu
instance_of: Mountain
countries: Bolivia
coordinates: lat: -19.43333333
lon: -67.38333333
surface_form: ch'iyar qullu
instance_of: Mountain
countries: Bolivia
coordinates: lat: -19.43333333
lon: -67.38333333
surface_form: ch'iyar qullu
instance_of: Mountain
countries: Bolivia
coordinates: lat: -16.5044
lon: -67.975
surface_form: ch'iyar qullu
instance_of: Mountain
countries: Bolivia
coordinates: lat: -16.5044
lon: -67.975
surface_form: ch'iyar qullu
instance_of: Mountain
countries: Bolivia
coordinates: lat: -16.2556
lon: -68.2831
surface_form: ch'iyar qullu
instance_of: Mountain
countries: Bolivia
coordinates: lat: -16.2556
lon: -68.2831
surface_form: tata ch'iyar qullu
instance_of: Mountain
countries: Bolivia
coordinates: lat: -16.50222222
lon: -67.94166667
It inhabits open grassy slopes and is on the wing from November until January. Taxonomy. This species was first described by Edward Meyrick in 1883 using specimens he collected near Lake Wakatipu in December. He originally named the species &quot;Oecophora homodoxa&quot;. Meyrick went on to give a fuller description of the species in 1884.

Geographic entities mentioned:
surface_form: Lake Wakatipu
instance_of: Lake
countries: New Zealand
coordinates: lat: -45.085
lon: 168.561
Daggett Brook Township, Crow Wing County, Minnesota. Daggett Brook Township is a township in Crow Wing County, Minnesota, United States. The population was 448 at the 2000 census. This township took its name from Daggett Brook. Geography. According to the United States Census Bureau, the township has a total area of, of which is land and (0.22%) is water. Demographics.

Geographic entities mentioned:
surface_form: Daggett Brook
instance_of: Watercourse
countries: United States
coordinates: lat: 46.24302
lon: -94.12166
Winona Lake (Flathead County, Montana). Winona Lake is located in Glacier National Park, in the U. S. state of Montana. Winona Lake is west of Logging Lake.

Geographic entities mentioned:
surface_form: Logging Lake
instance_of: Lake
countries: United States
coordinates: lat: 48.7531
lon: -114.089
surface_form: winona lake
instance_of: Lake
countries: United States
coordinates: lat: 48.7294
lon: -114.236
Winona Lake (Flathead County, Montana). Winona Lake is located in Glacier National Park, in the U. S. state of Montana. Winona Lake is west of Logging Lake.

Geographic entities mentioned:
surface_form: winona lake (flathead county, montana)
instance_of: Lake
countries: United States
coordinates: lat: 48.7294
lon: -114.236
Winona Lake (Flathead County, Montana). Winona Lake is located in Glacier National Park, in the U. S. state of Montana. Winona Lake is west of Logging Lake.

Geographic entities mentioned:
surface_form: winona lake
instance_of: Lake
countries: United States
coordinates: lat: 48.7294
lon: -114.236
Moel Llyfnant. Moel Llyfnant is a mountain in the southern portion of the Snowdonia National Park in Gwynedd, Wales. It is a peak in the Arenig mountain range. It lies to the west of Arenig Fawr. It has one notable top, the twin peaked Gallt y Daren, being at the end of its west ridge. The summit area has rocky outcrops, on top of one lies the small cairn that marks the summit.

Geographic entities mentioned:
surface_form: Arenig Fawr
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 52.917125
lon: -3.745937
Moel Llyfnant. Moel Llyfnant is a mountain in the southern portion of the Snowdonia National Park in Gwynedd, Wales. It is a peak in the Arenig mountain range. It lies to the west of Arenig Fawr. It has one notable top, the twin peaked Gallt y Daren, being at the end of its west ridge. The summit area has rocky outcrops, on top of one lies the small cairn that marks the summit.

Geographic entities mentioned:
surface_form: Gallt y Daren
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 52.89375
lon: -3.81709
It lies to the west of Arenig Fawr. It has one notable top, the twin peaked Gallt y Daren, being at the end of its west ridge. The summit area has rocky outcrops, on top of one lies the small cairn that marks the summit. The views of Arenig Fawr are excellent, while to the south Rhobell Fawr and Dduallt can be observed, and to the west Gallt y Daren and Foel Boeth.

Geographic entities mentioned:
surface_form: Arenig Fawr
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 52.917125
lon: -3.745937
surface_form: Rhobell Fawr
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 52.814
lon: -3.802
surface_form: Dduallt
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 52.830197222222
lon: -3.7657777777778
surface_form: Gallt y Daren
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 52.89375
lon: -3.81709
Moel Llyfnant. Moel Llyfnant is a mountain in the southern portion of the Snowdonia National Park in Gwynedd, Wales. It is a peak in the Arenig mountain range. It lies to the west of Arenig Fawr. It has one notable top, the twin peaked Gallt y Daren, being at the end of its west ridge. The summit area has rocky outcrops, on top of one lies the small cairn that marks the summit.

Geographic entities mentioned:
surface_form: moel llyfnant
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 52.900833333333
lon: -3.7730555555556
Erongo Region. Erongo is one of the 14 regions of Namibia. The capital is Swakopmund. It is named after Mount Erongo, a well-known landmark in Namibia and in this area. Erongo contains the municipalities of Walvis Bay, Swakopmund, Henties Bay and Omaruru, as well as the towns Arandis, Karibib and Usakos. All the main centres within this region are connected by paved roads.

Geographic entities mentioned:
surface_form: Mount Erongo
instance_of: Mountain
countries: Namibia
Mount Fury. Mount Fury, elevation, is in North Cascades National Park in the U.S. state of Washington. Several small glaciers are on the slopes of Mount Fury, and it is the second tallest peak in the Picket Range, after Luna Peak which lies to the northeast. Climate. Mount Fury is located in the marine west coast climate zone of western North America.

Geographic entities mentioned:
surface_form: washington
instance_of: Lake
countries: United States
coordinates: lat: 47.616666666667
lon: -122.26472222222
surface_form: mount fury
instance_of: Mountain
countries: United States
coordinates: lat: 48.8122
lon: -121.323
Mount Fury. Mount Fury, elevation, is in North Cascades National Park in the U.S. state of Washington. Several small glaciers are on the slopes of Mount Fury, and it is the second tallest peak in the Picket Range, after Luna Peak which lies to the northeast. Climate. Mount Fury is located in the marine west coast climate zone of western North America.

Geographic entities mentioned:
surface_form: mount fury
instance_of: Mountain
countries: United States
coordinates: lat: 48.8122
lon: -121.323