Sarmila/GeoWiki-Features huggingface dataset:
The park was designed by E. J. Johnson, who would later serve as park superintendent from 1935 to 1940. The design of structures and facilities employed the same National Park Service rustic style that had been used previously at Yellowstone, Grand Canyon and Yosemite National Parks. Lake Murray State Park Lodge became the first of seven state-owned resort lodges in 1951.

Geographic entities mentioned:
surface_form: yosemite
instance_of: Valley
countries: United States
coordinates: lat: 37.721694444444445
lon: -119.646
surface_form: grand canyon
instance_of: Valley
countries: United States
coordinates: lat: 38.65888889
lon: -91.10388889
Lake Murray (Oklahoma). Lake Murray is a lake in south central Oklahoma, near Ardmore named for Oklahoma Governor William H. Murray. It was created by damming Anadarche and Fourche Maline Creeks. The lake is wholly within Lake Murray State Park, Oklahoma's largest state park, containing over 12,500 acres (51 km2) of relative wilderness.

Geographic entities mentioned:
surface_form: lake murray (oklahoma)
instance_of: Lake
countries: United States
coordinates: lat: 34.0496
lon: -97.0721
Lake Murray (Oklahoma). Lake Murray is a lake in south central Oklahoma, near Ardmore named for Oklahoma Governor William H. Murray. It was created by damming Anadarche and Fourche Maline Creeks. The lake is wholly within Lake Murray State Park, Oklahoma's largest state park, containing over 12,500 acres (51 km2) of relative wilderness.

Geographic entities mentioned:
surface_form: lake murray
instance_of: Lake
countries: United States
coordinates: lat: 34.0496
lon: -97.0721
Murray. It was created by damming Anadarche and Fourche Maline Creeks. The lake is wholly within Lake Murray State Park, Oklahoma's largest state park, containing over 12,500 acres (51 km2) of relative wilderness. A state-operated lodge and resort is located on the west shore that serves many visitors to the lake, and serves as a base for numerous cabin and campground facilities near the lake.

Geographic entities mentioned:
surface_form: lake murray
instance_of: Lake
countries: United States
coordinates: lat: 34.0496
lon: -97.0721
A state-operated lodge and resort is located on the west shore that serves many visitors to the lake, and serves as a base for numerous cabin and campground facilities near the lake. On October 12, 2001, Lake Murray State Park became the first Oklahoma state park listed on the National Register of Historic Places. Park history.

Geographic entities mentioned:
surface_form: lake murray
instance_of: Lake
countries: United States
coordinates: lat: 34.0496
lon: -97.0721
1933, to purchase about in Carter and Love Counties for a state park. The park and the man-made lake it contained would be named Lake Murray, for William H. &quot;Alfalfa Bill&quot; Murray, who was Oklahoma governor from 1931 until 1936. During the following year, the National Park Service (NPS) acquired adjacent to Lake Murray State Park.

Geographic entities mentioned:
surface_form: lake murray
instance_of: Lake
countries: United States
coordinates: lat: 34.0496
lon: -97.0721
The park and the man-made lake it contained would be named Lake Murray, for William H. &quot;Alfalfa Bill&quot; Murray, who was Oklahoma governor from 1931 until 1936. During the following year, the National Park Service (NPS) acquired adjacent to Lake Murray State Park. The land purchased was designated as a Recreational Demonstration Area (RDA).

Geographic entities mentioned:
surface_form: lake murray
instance_of: Lake
countries: United States
coordinates: lat: 34.0496
lon: -97.0721
&quot;Alfalfa Bill&quot; Murray, who was Oklahoma governor from 1931 until 1936. During the following year, the National Park Service (NPS) acquired adjacent to Lake Murray State Park. The land purchased was designated as a Recreational Demonstration Area (RDA). The Civilian Conservation Corps (CCC), established two camps to support the Lake Murray project. The park was designed by E. J.

Geographic entities mentioned:
surface_form: lake murray
instance_of: Lake
countries: United States
coordinates: lat: 34.0496
lon: -97.0721
Lake Murray State Park Lodge became the first of seven state-owned resort lodges in 1951. In 2013, the state governor authorized the Department of Tourism to spend up to $15 million to construct a new lodge at Lake Murray State Park. After a number of changes, upgrades and cost overruns, the new lodge was completed in 2017 at a cost of over $30 million. Park description.

Geographic entities mentioned:
surface_form: lake murray
instance_of: Lake
countries: United States
coordinates: lat: 34.0496
lon: -97.0721
Park description. Lake Murray State Park is Oklahoma's oldest and largest state park. The state legislature bought the property for the park for about $490,000 on April 10, 1933. Workers in two Emergency Works Act programs established during the height of the Depression by then-President Franklin D.

Geographic entities mentioned:
surface_form: lake murray
instance_of: Lake
countries: United States
coordinates: lat: 34.0496
lon: -97.0721
It had been built based on photographs of a European castle taken during World War I by veteran Sen. Fred Tucker, a local legislator for whom the tower is named. Fishing, boating and all water sports are allowed at Lake Murray. Lake Murray Lodge offers guest rooms and suites, cabins, meeting space, The Apple Bin restaurant, and the Parlor.

Geographic entities mentioned:
surface_form: lake murray
instance_of: Lake
countries: United States
coordinates: lat: 34.0496
lon: -97.0721
surface_form: lake murray
instance_of: Lake
countries: United States
coordinates: lat: 34.0496
lon: -97.0721
Other facilities found in the park include an airstrip, Boat Mechanic, marina with rentals, swimming pool with a changing house, swimming beach, riding stable, remote control air field for hobbyists, miniature golf course and Frisbee golf. Nine RV campgrounds with over 300 RV sites and unlimited tent sites are located throughout Lake Murray State Park with full hookups, restrooms and showers.

Geographic entities mentioned:
surface_form: lake murray
instance_of: Lake
countries: United States
coordinates: lat: 34.0496
lon: -97.0721
surface_form: lake murray
instance_of: Lake
countries: United States
coordinates: lat: 34.0496
lon: -97.0721
Lake Murray State Park was the first Oklahoma state park listed on the National Register of Historic Places. In 2001, National Public Radio reported that Lake Murray State Park was Oklahoma's most popular state park, attracting over 1.7 million visitors, and that it earned the most money from activity fees. Including Lake Murray lodge, the park generated nearly $3.2 million for the year.

Geographic entities mentioned:
surface_form: lake murray
instance_of: Lake
countries: United States
coordinates: lat: 34.0496
lon: -97.0721
surface_form: lake murray
instance_of: Lake
countries: United States
coordinates: lat: 34.0496
lon: -97.0721
In 2001, National Public Radio reported that Lake Murray State Park was Oklahoma's most popular state park, attracting over 1.7 million visitors, and that it earned the most money from activity fees. Including Lake Murray lodge, the park generated nearly $3.2 million for the year. Lake description.

Geographic entities mentioned:
surface_form: lake murray
instance_of: Lake
countries: United States
coordinates: lat: 34.0496
lon: -97.0721
It is just one of the many exhibits at Tucker Tower Nature Center. Other displays include the reconstructed skull and fossilized bones of a mastodon found along the Washita River about 35 miles away; a mind-boggling animal skull collection, and educational exhibits of fossils, Lake Murray history, insects, fish and wildlife, legends, and rock specimens.

Geographic entities mentioned:
surface_form: lake murray
instance_of: Lake
countries: United States
coordinates: lat: 34.0496
lon: -97.0721
Fruita is a part of the Grand Junction, Colorado Metropolitan Statistical Area and lies within the Grand Valley. The geography is identified by the bordering Colorado River (historically known as the Grand River) on the southern edge of the town, the Uncompahgre Plateau known for its pinyon-juniper landscape, and the Book Cliffs range on the northern edge of the Grand Valley.

Geographic entities mentioned:
surface_form: Uncompahgre Plateau
instance_of: Plateau
countries: United States
coordinates: lat: 38.55
lon: -108.467
It currently is the home to the Fruita Civic Center. Geography. Fruita is located above sea level in the high desert climate zone on the Colorado Plateau. Surrounding the city limits is the Colorado River, the Colorado National Monument and the Book Cliffs range which extends west into the state of Utah north of Interstate 70.

Geographic entities mentioned:
surface_form: Colorado Plateau
instance_of: Plateau
countries: United States
coordinates: lat: 37
lon: -110
Rožično. Rožično () is a small dispersed settlement in the Tuhinj Valley in the Municipality of Kamnik in the Upper Carniola region of Slovenia. It lies along the side valley of Rožičnica Creek, a tributary of the Nevljica River.

Geographic entities mentioned:
surface_form: Tuhinj Valley
instance_of: Valley
countries: Slovenia
coordinates: lat: 46.221413888889
lon: 14.775925
In Irish myth and later folklore, the festivals of Samhain and Beltane (Bealtaine) are liminal times, when contact with the Otherworld was more likely. In the tales, the Otherworld is often reached by entering ancient burial mounds, such as those at Brú na Bóinne and Cnoc Meadha.

Geographic entities mentioned:
surface_form: Cnoc Meadha
instance_of: Mountain
countries: Ireland
coordinates: lat: 53.48186111
lon: -8.96054444
The mountain is located in Chaffee County, Colorado, and in the San Isabel National Forest. The mountain is named after Chipeta, a Native American leader known for her courageous efforts to mediate between Native Americans and European settlers. Nearby Mount Ouray, just southeast of Chipeta Mountain, is named after Chipeta's husband, Chief Ouray. Geology.

Geographic entities mentioned:
surface_form: Mount Ouray
instance_of: Mountain
countries: United States
coordinates: lat: 38.422777777778
lon: -106.22472222222
surface_form: chipeta mountain
instance_of: Mountain
countries: United States
coordinates: lat: 38.43944
lon: -106.24641
For unknown reasons, larger-scale maps of the region later published showed differently. The Bonanza, Colorado 1:62,500 scale maps first published in 1959 and the Mount Ouray, CO 1:24,000 scale maps first published in 1980 assigned the name Chipeta Mountain to a lower rise (elevation) on the southwest ridge of the mountain.

Geographic entities mentioned:
surface_form: mount ouray
instance_of: Mountain
countries: United States
coordinates: lat: 38.422777777778
lon: -106.22472222222
surface_form: chipeta mountain
instance_of: Mountain
countries: United States
coordinates: lat: 38.43944
lon: -106.24641
Chipeta Mountain. Chipeta Mountain is a mountain summit in the Sawatch Range of the Rocky Mountains of North America. The mountain is located in Chaffee County, Colorado, and in the San Isabel National Forest. The mountain is named after Chipeta, a Native American leader known for her courageous efforts to mediate between Native Americans and European settlers.

Geographic entities mentioned:
surface_form: a mountain
instance_of: Mountain
countries: United States
coordinates: lat: 32.2925
lon: -106.69777777778
surface_form: chipeta mountain
instance_of: Mountain
countries: United States
coordinates: lat: 38.43944
lon: -106.24641
These maps show the name Chipeta Mountain applied to the highest point of the mountain at an elevation of. Revisions of this map published through 1968 continued to label the high point as Chipeta Mountain. For unknown reasons, larger-scale maps of the region later published showed differently.

Geographic entities mentioned:
surface_form: high point
instance_of: Mountain
countries: United States
coordinates: lat: 41.924722222222
lon: -74.288055555556
surface_form: high point
instance_of: Mountain
countries: United States
coordinates: lat: 41.3209
lon: -74.6616
surface_form: chipeta mountain
instance_of: Mountain
countries: United States
coordinates: lat: 38.43944
lon: -106.24641
In 1963 the United States Board on Geographic Names (USBGN) accepted the name Chipeta Mountain and assigned it to this lower sub-peak. For over 50 years, the mountain's true summit remained officially unnamed. In 2017, the USBGN approved a citizen proposal to restore the name Chipeta Mountain to the mountain's high point.

Geographic entities mentioned:
surface_form: high point
instance_of: Mountain
countries: United States
coordinates: lat: 41.924722222222
lon: -74.288055555556
surface_form: high point
instance_of: Mountain
countries: United States
coordinates: lat: 41.3209
lon: -74.6616
surface_form: chipeta mountain
instance_of: Mountain
countries: United States
coordinates: lat: 38.43944
lon: -106.24641
Chipeta Mountain. Chipeta Mountain is a mountain summit in the Sawatch Range of the Rocky Mountains of North America. The mountain is located in Chaffee County, Colorado, and in the San Isabel National Forest. The mountain is named after Chipeta, a Native American leader known for her courageous efforts to mediate between Native Americans and European settlers.

Geographic entities mentioned:
surface_form: chipeta mountain
instance_of: Mountain
countries: United States
coordinates: lat: 38.43944
lon: -106.24641
Nearby Mount Ouray, just southeast of Chipeta Mountain, is named after Chipeta's husband, Chief Ouray. Geology. Chipeta Mountain is dominated by Paleoproterozoic gneisses. These dark rocks were subsequently intruded by magma, and lighter-colored igneous intrusions are visible on the ridges extending below the peak.

Geographic entities mentioned:
surface_form: chipeta mountain
instance_of: Mountain
countries: United States
coordinates: lat: 38.43944
lon: -106.24641
Erosion has removed the overlying sedimentary and volcanic rocks. Along the northeast flank of Chipeta Mountain are normal faults associated with the Rio Grande Rift. This rifting has resulted in extreme elevation gradients along the eastern side of the Sawatch Range. Chipeta Mountain looms over above the graben below.

Geographic entities mentioned:
surface_form: chipeta mountain
instance_of: Mountain
countries: United States
coordinates: lat: 38.43944
lon: -106.24641
This rifting has resulted in extreme elevation gradients along the eastern side of the Sawatch Range. Chipeta Mountain looms over above the graben below. Chipeta Mountain was glaciated, and the most prominent glacial cirques are located on the northeast and southeast sides of the mountain where tarns and glacial deposits are found. Climate.

Geographic entities mentioned:
surface_form: chipeta mountain
instance_of: Mountain
countries: United States
coordinates: lat: 38.43944
lon: -106.24641
Climate. Chipeta Mountain's climate is classified as a tundra climate (ET) in the Köppen system and more specifically as an alpine climate, with cold, snowy winters and cool summers. It receives precipitation as snow in winter and as thunderstorms in summer, with June typically being a drier month. Hiking.

Geographic entities mentioned:
surface_form: chipeta mountain
instance_of: Mountain
countries: United States
coordinates: lat: 38.43944
lon: -106.24641
Hiking. Hiking to the summit of Chipeta Mountain is typically done during the summer and early fall when snow is free of the roads used to reach the trailheads. The easiest route to the summit starts at the Marshall Pass Trailhead located on the Continental Divide south of the mountain. A hike along the Monarch Crest Trail and then Forest Trail 484 leads to the southwest ridge of the mountain.

Geographic entities mentioned:
surface_form: chipeta mountain
instance_of: Mountain
countries: United States
coordinates: lat: 38.43944
lon: -106.24641
From there, an off-trail, class 2 ridge hike leads northeast to the summit. This route has an elevation gain of. Chipeta Mountain can also be reached from four-wheel-drive roads and trails to the east. One route begins at the end of Little Cochetopa Road (Forest Road 710). Forest Trail 1409 leads west to the southwest ridge of the mountain, which can then be hiked to the summit.

Geographic entities mentioned:
surface_form: chipeta mountain
instance_of: Mountain
countries: United States
coordinates: lat: 38.43944
lon: -106.24641
2017 name change. The earliest United States Geological Survey topographic maps of the region were the Montrose, Colorado 1:250,000 scale maps first published in 1956. These maps show the name Chipeta Mountain applied to the highest point of the mountain at an elevation of. Revisions of this map published through 1968 continued to label the high point as Chipeta Mountain.

Geographic entities mentioned:
surface_form: chipeta mountain
instance_of: Mountain
countries: United States
coordinates: lat: 38.43944
lon: -106.24641
The Bonanza, Colorado 1:62,500 scale maps first published in 1959 and the Mount Ouray, CO 1:24,000 scale maps first published in 1980 assigned the name Chipeta Mountain to a lower rise (elevation) on the southwest ridge of the mountain. In 1963 the United States Board on Geographic Names (USBGN) accepted the name Chipeta Mountain and assigned it to this lower sub-peak.

Geographic entities mentioned:
surface_form: chipeta mountain
instance_of: Mountain
countries: United States
coordinates: lat: 38.43944
lon: -106.24641
Haas Glacier. Haas Glacier () is a steep tributary glacier draining northward from Rawson Plateau to enter the south side of Bowman Glacier, in the Queen Maud Mountains of Antarctica. It was mapped by the United States Geological Survey from surveys and U.S. Navy air photos, 1960–64, and was named by the Advisory Committee on Antarctic Names for Charles G.

Geographic entities mentioned:
surface_form: Rawson Plateau
instance_of: Mountain
coordinates: lat: -85.8667
lon: -164.75
Big Lake (Texas). Big Lake is an intermittent dry lake located one-mile (1.6 km) south and southwest of the city of Big Lake in Reagan County, Texas. Covering approximately, the playa lies in a floodplain and is fed primarily by Big Lake Draw and a number of other, unnamed smaller draws. Scrub brush, mesquite, juniper, grasses, and water-tolerant hardwoods grow around the lake.

Geographic entities mentioned:
surface_form: big lake
instance_of: Lake
countries: United States
coordinates: lat: 40.0725
lon: -95.345
surface_form: big lake
instance_of: Lake
countries: United States
coordinates: lat: 45.1722398
lon: -67.6821052
surface_form: big lake
instance_of: Lake
countries: United States
coordinates: lat: 45.819722222222
lon: -96.113055555556
surface_form: big lake
instance_of: Lake
countries: United States
coordinates: lat: 31.1667
lon: -101.483
surface_form: big lake
instance_of: Lake
countries: United States
coordinates: lat: 33.8847
lon: -109.415
Big Lake (Texas). Big Lake is an intermittent dry lake located one-mile (1.6 km) south and southwest of the city of Big Lake in Reagan County, Texas. Covering approximately, the playa lies in a floodplain and is fed primarily by Big Lake Draw and a number of other, unnamed smaller draws. Scrub brush, mesquite, juniper, grasses, and water-tolerant hardwoods grow around the lake.

Geographic entities mentioned:
surface_form: big lake
instance_of: Lake
countries: United States
coordinates: lat: 40.0725
lon: -95.345
surface_form: big lake
instance_of: Lake
countries: United States
coordinates: lat: 40.0725
lon: -95.345
surface_form: big lake
instance_of: Lake
countries: United States
coordinates: lat: 45.1722398
lon: -67.6821052
surface_form: big lake
instance_of: Lake
countries: United States
coordinates: lat: 45.1722398
lon: -67.6821052
surface_form: big lake
instance_of: Lake
countries: United States
coordinates: lat: 45.819722222222
lon: -96.113055555556
surface_form: big lake
instance_of: Lake
countries: United States
coordinates: lat: 45.819722222222
lon: -96.113055555556
surface_form: dry lake
instance_of: Lake
countries: United States
coordinates: lat: 44.6282988
lon: -97.0561783
surface_form: dry lake
instance_of: Lake
countries: United States
coordinates: lat: 38.3360373
lon: -117.7898285
surface_form: dry lake
instance_of: Lake
countries: United States
coordinates: lat: 45.0425
lon: -97.31972222
surface_form: big lake
instance_of: Lake
countries: United States
coordinates: lat: 31.1667
lon: -101.483
surface_form: big lake
instance_of: Lake
countries: United States
coordinates: lat: 31.1667
lon: -101.483
surface_form: big lake
instance_of: Lake
countries: United States
coordinates: lat: 33.8847
lon: -109.415
surface_form: big lake
instance_of: Lake
countries: United States
coordinates: lat: 33.8847
lon: -109.415
Conception. The Gobbins cliff path was the brainchild of a pioneering Irish railway engineer called Berkeley Deane Wise. Originally from New Ross, Wise served his apprenticeship working on the railway line between Dublin and Wexford. At the age of just 22, he developed tunnels and bridges for one of the most challenging sections in the country, along the coast at Bray Head.

Geographic entities mentioned:
surface_form: Bray Head
instance_of: Mountain
countries: Ireland
coordinates: lat: 53.190527777778
lon: -6.0841666666667
Tourism NI has contributed funding towards the cliff-top path, and a platform and staircase were funded by the North East Region Rural Development Programme. The Gobbins project is part of a cross-border project which also includes the enhancement of another tourist destination based in Sliabh Liag, County Donegal.

Geographic entities mentioned:
surface_form: Sliabh Liag
instance_of: Mountain
countries: Ireland
coordinates: lat: 54.638055555556
lon: -8.6813888888889
By 1870 the colony had 6500 inhabitants. Chile. From 1850 to 1875 the region around Valdivia, Osorno and Llanquihue in Southern Chile received some 6,000 German immigrants as part of a state-led colonization scheme. Some immigrants were leaving Europe as consequence of the aftermath of the German revolutions of 1848–49.

Geographic entities mentioned:
surface_form: Llanquihue
instance_of: Lake
countries: Chile
coordinates: lat: -41.133333333333
lon: -72.783333333333
The Nabi Saeen Mosque (;) is a mosque located on Nabi Saeen Hill in Nazareth, in northern Israel. The mosque is located at the top of the ridge enclosing the city from the north, approximately north of the Salesian Basilica of Jesus the Adolescent, providing a panoramic view of Nazareth and the Jezreel Valley to the south, and the Upper Galilee and Haifa outskirts (Krayot) to the north and west.

Geographic entities mentioned:
surface_form: Jezreel Valley
instance_of: Valley
countries: Israel
coordinates: lat: 32.596388888889
lon: 35.241944444444
It contains the civil parishes of Killearnan, Knockbain, Avoch, Rosemarkie, Cromarty, Resolis, and Urquhart. These parishes had a total population of 12,302 at the 2011 census. The northern slopes of the Black Isle offer fine views of Dingwall, Ben Wyvis, Fyrish and the deepwater anchorage at Invergordon. To the south, Inverness and the Monadhliath Mountains can be seen. Description.

Geographic entities mentioned:
surface_form: Ben Wyvis
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 57.679119444444
lon: -4.5792194444444
Both were designed by Ossian Cole Simonds, the father of Prairie School landscape architecture. The parkway runs parallel with the Yahara River, leading to the park where the river meets Lake Mendota. In 1999, the park and parkway were successfully nominated and listed on the State and the National Register of Historic Places. History.

Geographic entities mentioned:
surface_form: Lake Mendota
instance_of: Lake
countries: United States
coordinates: lat: 43.106666666667
lon: -89.424722222222
In 1999, the park and parkway were successfully nominated and listed on the State and the National Register of Historic Places. History. Before White settlement, when the Four Lakes region was home to Native Americans, the Yahara River meandered from Lake Mendota
through marsh and swamps, across the isthmus to Lake Monona. In 1849 future governor Leonard J.

Geographic entities mentioned:
surface_form: Lake Monona
instance_of: Lake
countries: United States
coordinates: lat: 43.069166666667
lon: -89.359444444444
The quartzites are often nearly pure quartz, which is puzzling for sediments which must have eroded from igneous rock. Their purity may reflect unusual conditions of chemical weathering, at a time when the Earth's atmosphere was beginning to be oxygenated. In Ireland areas of quartzite are found across the west and northwest, with Errigal in County Donegal as the most prominent outcrop.

Geographic entities mentioned:
surface_form: Errigal
instance_of: Mountain
countries: Ireland
coordinates: lat: 55.033
lon: -8.112
A good example of a quartzite area is on the Corraun Peninsula in County Mayo, which has a very thin layer of Irish Atlantic Bog covering it. In the United Kingdom, a craggy ridge of quartzite called the Stiperstones (early Ordovician – Arenig Epoch, 500 Ma) runs parallel with the Pontesford-Linley fault, 6 km north-west of the Long Mynd in south Shropshire.

Geographic entities mentioned:
surface_form: Stiperstones
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 52.581944444444
lon: -2.935
surface_form: Long Mynd
instance_of: Plateau
countries: United Kingdom
coordinates: lat: 52.5478
lon: -2.8389
In the United Kingdom, a craggy ridge of quartzite called the Stiperstones (early Ordovician – Arenig Epoch, 500 Ma) runs parallel with the Pontesford-Linley fault, 6 km north-west of the Long Mynd in south Shropshire. Also to be found in England are the Cambrian &quot;Wrekin quartzite&quot; (in Shropshire), and the Cambrian &quot;Hartshill quartzite&quot; (Nuneaton area).

Geographic entities mentioned:
surface_form: Wrekin
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 52.66916666666667
lon: -2.551388888888889
In Wales, Holyhead Mountain and most of Holy island off Anglesey sport excellent Precambrian quartzite crags and cliffs. In the Scottish Highlands, several mountains (e.g. Foinaven, Arkle) composed of Cambrian quartzite can be found in the far north-west Moine Thrust Belt running in a narrow band from Loch Eriboll in a south-westerly direction to Skye.

Geographic entities mentioned:
surface_form: Foinaven
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 58.4121
lon: -4.8860305555556
Deposits are also quarried in Kragerø Municipality, and several other deposits are known but not actively quarried. The highest mountain in Mozambique, Monte Binga (2436 m), as well as the rest of the surrounding Chimanimani Plateau are composed of very hard, pale grey, Precambrian quartzite. Quartzite is also mined in Brazil for use in kitchen countertops. Uses.

Geographic entities mentioned:
surface_form: Monte Binga
instance_of: Mountain
countries: Mozambique
coordinates: lat: -19.774166666667
lon: 33.060555555556
To the southwest, it extends to the Kriva River in North Macedonia. The highest summit of Kraishte is the Besna Kobila mountain in Serbia (1,922 m); the border mountain of Karvav Kamak includes the highest point of the region in Bulgaria, Bilo (1,737 m).

Geographic entities mentioned:
surface_form: Besna Kobila
instance_of: Mountain
countries: Serbia
coordinates: lat: 42.529444444444
lon: 22.230555555556
surface_form: Karvav Kamak
instance_of: Mountain
countries: Bulgaria
coordinates: lat: 42.683
lon: 22.466
The Bulgarian part of the region includes 23 small mountain ranges in two grouping: the Ruy-Verila range encompassing Miloslavska planina (1,485 m), Ruy (1,706 m), Ezdimirska Planina (1,219 m), Strazha (1,385 m), Lyubash (1,398 m), Bohovska planina (1,318 m), Karvav Kamak (1,737 m), Leshnikovska Planina (1,086 m), Elovishka Planina (1,329 m), Penkyovska Planina (1,187 m), Lyulyak (1,324 m), Erulska Planina (1,481 m), Cherna Gora (1,129 m), Golo Bardo (1,158 m) and Verila (1,415 m) and the Milevsko-Konyavska range consisting of Milevska planina (1,733 m), Izvorska Planina (1,243 m), Kobilska Planina (1,356 m), Chudinska Planina (1,497 m), Lisets (1,500 m), Zemenska Planina (1,295 m), Rudina Planina (1,172 m) and Konyavska Planina (1,487 m).

Geographic entities mentioned:
surface_form: Miloslavska planina
instance_of: Mountain
countries: Bulgaria
Serbia
coordinates: lat: 42.825
lon: 22.4397
surface_form: Ezdimirska Planina
instance_of: Mountain
countries: Bulgaria
coordinates: lat: 42.815
lon: 22.702
surface_form: Lyubash
instance_of: Mountain
countries: Bulgaria
coordinates: lat: 42.756
lon: 22.754
surface_form: Bohovska planina
instance_of: Mountain
countries: Bulgaria
Serbia
coordinates: lat: 42.7419
lon: 22.5003
surface_form: Leshnikovska Planina
instance_of: Mountain
countries: Bulgaria
coordinates: lat: 42.784
lon: 22.574
surface_form: Elovishka Planina
instance_of: Mountain
countries: Bulgaria
coordinates: lat: 42.709
lon: 22.562
surface_form: Verila
instance_of: Mountain
countries: Bulgaria
coordinates: lat: 42.391666666667
lon: 23.263611111111
surface_form: Milevska planina
instance_of: Mountain
countries: Serbia
Bulgaria
coordinates: lat: 42.565
lon: 22.43944444
surface_form: Izvorska Planina
instance_of: Mountain
countries: Bulgaria
Serbia
coordinates: lat: 42.508
lon: 22.546
surface_form: Kobilska Planina
instance_of: Mountain
countries: Bulgaria
coordinates: lat: 42.513
lon: 22.61
surface_form: Chudinska Planina
instance_of: Mountain
countries: Bulgaria
Serbia
coordinates: lat: 42.3686
lon: 22.4656
Sundvollen. Sundvollen is a village in the municipality of Hole, in the county of Buskerud, Norway. Sundvollen is located along the east side of Tyrifjorden where the E16 crosses west over Steinsfjorden, the northeastern arm of Tyrifjorden, to Kroksund. The village had 801 inhabitants as of January 2009.

Geographic entities mentioned:
surface_form: Tyrifjorden
instance_of: Lake
countries: Norway
coordinates: lat: 60.033333333333
lon: 10.133333333333
surface_form: Steinsfjorden
instance_of: Body of water
countries: Norway
coordinates: lat: 60.0833
lon: 10.3167
This unique area was formed after the last ice age when the continental glacier melted leaving behind a large lake called Lake Warren. Over time, this lake was gradually reduced to present day Lake Erie and left behind a large tract of sandy soil to the west. The area was frequented by wildfires that only the thick-barked oak trees could survive.

Geographic entities mentioned:
surface_form: Lake Erie
instance_of: Lake
countries: Canada
United States
coordinates: lat: 42.25
lon: -80.99972222222222
Edward Island (Lake Superior). Edward Island is an island in Lake Superior, located southwest of the Black Bay Peninsula in Thunder Bay District, Northwestern Ontario. It is located about from Porphyry Island Provincial Park, about from Sleeping Giant Provincial Park and east of Silver Islet, Ontario. The island is about east of the city of Thunder Bay.

Geographic entities mentioned:
surface_form: Lake Superior
instance_of: Lake
countries: Canada
United States
coordinates: lat: 47.52881611111111
lon: -87.76002194444445
Umboi Island. Umboi (also named Rooke or Siassi) is a volcanic island between the mainland of Papua New Guinea and the island of New Britain. It is separated from New Britain by the Dampier Strait, and Huon Peninsula and New Guinea by the Vitiaz Strait. It has an elevation of. The Siassi Archipelago lies off the southeast coast of Umboi Island (a total of 18 islands, only seven are inhabited).

Geographic entities mentioned:
surface_form: umboi island
instance_of: Mountain
countries: Papua New Guinea
coordinates: lat: -5.6118861111111
lon: 147.88353055556
Umboi Island. Umboi (also named Rooke or Siassi) is a volcanic island between the mainland of Papua New Guinea and the island of New Britain. It is separated from New Britain by the Dampier Strait, and Huon Peninsula and New Guinea by the Vitiaz Strait. It has an elevation of. The Siassi Archipelago lies off the southeast coast of Umboi Island (a total of 18 islands, only seven are inhabited).

Geographic entities mentioned:
surface_form: umboi
instance_of: Mountain
countries: Papua New Guinea
coordinates: lat: -5.6118861111111
lon: 147.88353055556
It is separated from New Britain by the Dampier Strait, and Huon Peninsula and New Guinea by the Vitiaz Strait. It has an elevation of. The Siassi Archipelago lies off the southeast coast of Umboi Island (a total of 18 islands, only seven are inhabited). History. During the mid-1920s, the population of the Siassi Islands was a little over 700 people.

Geographic entities mentioned:
surface_form: umboi island
instance_of: Mountain
countries: Papua New Guinea
coordinates: lat: -5.6118861111111
lon: 147.88353055556
It extends 3.5 km in east-west direction and 2.5 km in north-south direction, is bounded to the west by Veleka Ridge, to the north by Arda Peak, Gerov Pass and Shumen Peak, and to the east by Yambol Peak, and flows southeastwards into Bransfield Strait east of Botev Point and west of Gela Point.

Geographic entities mentioned:
surface_form: Veleka Ridge
instance_of: Mountain
coordinates: lat: -62.74225
lon: -60.309444444444
surface_form: Yambol Peak
instance_of: Mountain
coordinates: lat: -62.740361111111
lon: -60.236388888889
surface_form: Bransfield Strait
instance_of: Body of water
countries: Antarctica
coordinates: lat: -63
lon: -59
Tarnovo Ice Piedmont. Tarnovo Ice Piedmont (,) is an ice piedmont on Rozhen Peninsula, Livingston Island in the South Shetland Islands, Antarctica is situated southeast of Charity Glacier and west-southwest of Prespa Glacier.

Geographic entities mentioned:
surface_form: tarnovo ice piedmont
instance_of: Landform
coordinates: lat: -62.7486
lon: -60.2694
Tarnovo Ice Piedmont. Tarnovo Ice Piedmont (,) is an ice piedmont on Rozhen Peninsula, Livingston Island in the South Shetland Islands, Antarctica is situated southeast of Charity Glacier and west-southwest of Prespa Glacier.

Geographic entities mentioned:
surface_form: tarnovo ice piedmont
instance_of: Landform
coordinates: lat: -62.7486
lon: -60.2694
surface_form: charity
instance_of: Mountain
coordinates: lat: -69.9
lon: -64.5667
Rock Island State Park (Wisconsin). Rock Island State Park is a state park of Wisconsin located on Rock Island off the tip of the Door Peninsula at the eastern edge of Green Bay and Lake Michigan. History. Rock Island was proposed as a state park in early 1961 by officials of the Town of Washington Island, particularly Jack Hagen the town chairman.

Geographic entities mentioned:
surface_form: Lake Michigan
instance_of: Lake
countries: United States
coordinates: lat: 44.007874
lon: -86.756451
Mount Pisgah (Massachusetts). Mount Pisgah is the highest point in Northborough, Massachusetts. Trails. The summit is marked at the intersection of the Summit Trail and the Tyler Trail. Look for the cairn, the marker is to the right.

Geographic entities mentioned:
surface_form: mount pisgah
instance_of: Mountain
countries: United States
coordinates: lat: 44.306111111111
lon: -70.023888888889
surface_form: mount pisgah
instance_of: Mountain
countries: United States
coordinates: lat: 42.377222222222
lon: -74.245
surface_form: mount pisgah
instance_of: Mountain
countries: United States
coordinates: lat: 42.3653
lon: -71.6578
surface_form: mount pisgah
instance_of: Mountain
countries: United States
coordinates: lat: 44.7297
lon: -72.0308
surface_form: mount pisgah
instance_of: Mountain
countries: United States
coordinates: lat: 41.8098
lon: -76.7159
surface_form: mount pisgah
instance_of: Mountain
countries: United States
coordinates: lat: 35.4255
lon: -82.7569
surface_form: mount pisgah
instance_of: Mountain
countries: United States
coordinates: lat: 40.86944444444445
lon: -75.74972222222222
surface_form: mount pisgah
instance_of: Mountain
countries: United States
coordinates: lat: 44.340833333333
lon: -74.128055555556
surface_form: mount pisgah
instance_of: Mountain
countries: United States
coordinates: lat: 39.996388888889
lon: -76.548888888889
surface_form: mount pisgah
instance_of: Mountain
countries: United States
coordinates: lat: 42.221111111111
lon: -74.735833333333
Trails. The summit is marked at the intersection of the Summit Trail and the Tyler Trail. Look for the cairn, the marker is to the right. In June 2005, under a stewardship agreement with MassWildlife, the Northborough Trails committee took over maintenance of about three miles (5 km) of recently developed trails on the MassWildlife property located on the south end of Mt. Pisgah.

Geographic entities mentioned:
surface_form: mt. pisgah
instance_of: Mountain
countries: United States
coordinates: lat: 44.306111111111
lon: -70.023888888889
surface_form: mt. pisgah
instance_of: Mountain
countries: United States
coordinates: lat: 42.377222222222
lon: -74.245
surface_form: mt. pisgah
instance_of: Mountain
countries: United States
coordinates: lat: 42.3653
lon: -71.6578
surface_form: mt. pisgah
instance_of: Mountain
countries: United States
coordinates: lat: 41.8098
lon: -76.7159
surface_form: mt. pisgah
instance_of: Mountain
countries: United States
coordinates: lat: 35.4255
lon: -82.7569
surface_form: mt. pisgah
instance_of: Mountain
countries: United States
coordinates: lat: 44.340833333333
lon: -74.128055555556
surface_form: mt. pisgah
instance_of: Mountain
countries: United States
coordinates: lat: 39.996388888889
lon: -76.548888888889
surface_form: mt. pisgah
instance_of: Mountain
countries: United States
coordinates: lat: 42.221111111111
lon: -74.735833333333
All motorized vehicles, including ATVs, are prohibited from MassWildlife property. In 2006 a new map of the Mt. Pisgah Conservation Area was completed by the Sudbury Valley Trustees. The map shows all the trails open to the public's use from the MassWildlife land on the south side of Mt. Pisgah to Linden Street in Berlin on the north side. Directions.

Geographic entities mentioned:
surface_form: mt. pisgah
instance_of: Mountain
countries: United States
coordinates: lat: 44.306111111111
lon: -70.023888888889
surface_form: mt. pisgah
instance_of: Mountain
countries: United States
coordinates: lat: 42.377222222222
lon: -74.245
surface_form: mt. pisgah
instance_of: Mountain
countries: United States
coordinates: lat: 42.3653
lon: -71.6578
surface_form: mt. pisgah
instance_of: Mountain
countries: United States
coordinates: lat: 41.8098
lon: -76.7159
surface_form: mt. pisgah
instance_of: Mountain
countries: United States
coordinates: lat: 35.4255
lon: -82.7569
surface_form: mt. pisgah
instance_of: Mountain
countries: United States
coordinates: lat: 44.340833333333
lon: -74.128055555556
surface_form: mt. pisgah
instance_of: Mountain
countries: United States
coordinates: lat: 39.996388888889
lon: -76.548888888889
surface_form: mt. pisgah
instance_of: Mountain
countries: United States
coordinates: lat: 42.221111111111
lon: -74.735833333333
Wallarobba Shire. Wallarobba Shire was a local government area in the Hunter region of New South Wales, Australia. Wallarobba Shire was proclaimed on 7 March 1906, one of 134 shires created after the passing of the &quot;Local Government (Shires) Act 1905&quot;. The shire office was in Dungog.

Geographic entities mentioned:
surface_form: Hunter
instance_of: Valley
countries: Australia
coordinates: lat: -32.56
lon: 151.17083333333332
Salinas River (California). The Salinas River (Rumsen: &quot;ua kot taiauačorx&quot;) is the longest river of the Central Coast region of California, running and draining. It flows north-northwest and drains the Salinas Valley that slices through the central California Coast Ranges south of Monterey Bay.

Geographic entities mentioned:
surface_form: Salinas Valley
instance_of: Valley
countries: United States
coordinates: lat: 36.7654
lon: -121.7918
Prehistory. People first appeared along the California coast approximately 13,000 years ago, during the latter part of the Pleistocene epoch. Up until European settlement in Alta California, the indigenous people who lived along the Salinas River were the Rumsen in the northern Salinas Valley, and the Salinan in the southern Salinas Valley.

Geographic entities mentioned:
surface_form: Salinas Valley
instance_of: Valley
countries: United States
coordinates: lat: 36.7654
lon: -121.7918
surface_form: Salinas Valley
instance_of: Valley
countries: United States
coordinates: lat: 36.7654
lon: -121.7918
It flows past Atascadero and Paso Robles (to Monterey). It receives the natural outflow of the Estrella River and the controlled outflows of the Nacimiento and San Antonio reservoirs through their respective river tributaries in southern Monterey County. The river passes through the active San Ardo Oil Field, and then into and through the Salinas Valley.

Geographic entities mentioned:
surface_form: Salinas Valley
instance_of: Valley
countries: United States
coordinates: lat: 36.7654
lon: -121.7918
Nyakagezi River. The Nyakagezi River () is a river in Burundi, a tributary of the Kinyankuru River. Course. The Nyakagezi rises in the south of the Sankinyinya &quot;colline&quot; of the Commune of Gahombo, Kayanza Province, and flows east. The RP52 road runs parallel to the river, south of it and north of the Ruvubu River, which also flows east.

Geographic entities mentioned:
surface_form: Kinyankuru River
instance_of: Watercourse
countries: Burundi
coordinates: lat: -3.08523
lon: 29.92609
surface_form: nyakagezi river
instance_of: Watercourse
countries: Burundi
coordinates: lat: -3.0032
lon: 29.9341
The RP52 road runs parallel to the river, south of it and north of the Ruvubu River, which also flows east. To the north of the Nyamugari Colline of the Commune of Ruhororo the Nyakagezi turns northeast. It continues east through marshes to the Kinyankuru River. It enters the Kinyankuru to the south of Rimiro &quot;colline&quot;. The Kinyankuru is in turn a tributary of the Ruvubu River.

Geographic entities mentioned:
surface_form: Kinyankuru River
instance_of: Watercourse
countries: Burundi
coordinates: lat: -3.08523
lon: 29.92609
surface_form: kinyankuru
instance_of: Watercourse
countries: Burundi
coordinates: lat: -3.08523
lon: 29.92609
Nyakagezi River. The Nyakagezi River () is a river in Burundi, a tributary of the Kinyankuru River. Course. The Nyakagezi rises in the south of the Sankinyinya &quot;colline&quot; of the Commune of Gahombo, Kayanza Province, and flows east. The RP52 road runs parallel to the river, south of it and north of the Ruvubu River, which also flows east.

Geographic entities mentioned:
surface_form: nyakagezi
instance_of: Watercourse
countries: Burundi
coordinates: lat: -3.0032
lon: 29.9341
The Nyakagezi rises in the south of the Sankinyinya &quot;colline&quot; of the Commune of Gahombo, Kayanza Province, and flows east. The RP52 road runs parallel to the river, south of it and north of the Ruvubu River, which also flows east. To the north of the Nyamugari Colline of the Commune of Ruhororo the Nyakagezi turns northeast. It continues east through marshes to the Kinyankuru River.

Geographic entities mentioned:
surface_form: nyakagezi
instance_of: Watercourse
countries: Burundi
coordinates: lat: -3.0032
lon: 29.9341
It enters the Kinyankuru to the south of Rimiro &quot;colline&quot;. The Kinyankuru is in turn a tributary of the Ruvubu River. Environment. The surroundings of Nyakagezi are a mosaic of agricultural land and natural vegetation. The area is densely populated, with 442 inhabitants per square kilometer as of 2016. The average annual temperature in the area is.

Geographic entities mentioned:
surface_form: nyakagezi
instance_of: Watercourse
countries: Burundi
coordinates: lat: -3.0032
lon: 29.9341
The wettest month is December, with an average of of precipitation, and the driest is July, with of precipitation. Agriculture. As of 2014 there were two managed marshes on the Nyakagezi, one of divided between the Commune of Gashikanwa and the Commune of Ngozi, and the other of in the Commune of Ngozi.

Geographic entities mentioned:
surface_form: nyakagezi
instance_of: Watercourse
countries: Burundi
coordinates: lat: -3.0032
lon: 29.9341
To the north of the Nyamugari Colline of the Commune of Ruhororo the Nyakagezi turns northeast. It continues east through marshes to the Kinyankuru River. It enters the Kinyankuru to the south of Rimiro &quot;colline&quot;. The Kinyankuru is in turn a tributary of the Ruvubu River. Environment. The surroundings of Nyakagezi are a mosaic of agricultural land and natural vegetation.

Geographic entities mentioned:
surface_form: kinyankuru
instance_of: Watercourse
countries: Burundi
coordinates: lat: -3.08523
lon: 29.92609
surface_form: kinyankuru
instance_of: Watercourse
countries: Burundi
coordinates: lat: -3.08523
lon: 29.92609
Ocean, Maryland. Ocean is an unincorporated community and census-designated place (CDP) in Allegany County, Maryland, United States. As of the 2010 census it had a population of 32. Ocean is located in the Georges Creek Valley of western Allegany County, along Maryland Route 936. Frostburg is to the north, and Lonaconing is to the southwest.

Geographic entities mentioned:
surface_form: Georges Creek Valley
instance_of: Valley
countries: United States
coordinates: lat: 39.5717
lon: -78.9772
In early spring, depending upon the precipitation, waterfalls may be seen on the edge of the canyons. Popular trails within the vicinity of the scenic drive loop include the Moenkopi Loop, Calico Hills, Calico Tanks, Turtlehead Mountain, Keystone Thrust, White Rock/La Madre Springs Loop, and the Ice Box Canyon trail. Wildfire history.

Geographic entities mentioned:
surface_form: Turtlehead Mountain
instance_of: Mountain
countries: United States
coordinates: lat: 36.180277777778
lon: -115.44611111111
Botanist Shannel Courtney, Department of Conservation's Technical Support Officer for Flora and Restoration and the 2008 Loder Cup recipient, stumbled upon a widespread growth of the species near a tributary of the Clarence River in January 2015, followed by reports of other specimens found in the Ruataniwha wetlands in the McKenzie Basin, and a third discovery in March in the Heron Basin in mid-Canterbury.

Geographic entities mentioned:
surface_form: Ruataniwha
instance_of: Lake
countries: New Zealand
coordinates: lat: -44.281
lon: 170.071
surface_form: Heron Basin
instance_of: Lake
countries: New Zealand
coordinates: lat: -43.479166666667
lon: 171.17194444444
The easternmost mile (1.6 km) of NY 100B was originally part of Route 2, an unsigned legislative route assigned by the New York State Legislature in 1908. The route began at the New York City line in Yonkers and went north through the eastern Hudson Valley to Valatie, where it ended at Route 1. Route 2 continued south from Dobbs Ferry Road on modern NY 100A and north on what is now NY 119.

Geographic entities mentioned:
surface_form: Hudson Valley
instance_of: Valley
countries: United States
coordinates: lat: 41.9209
lon: -73.9613
Debakcsy noted that there are several radio telescopes at Kitt Peak, such as the Very Long Baseline Array, but that telescope does not match the description given. DeBakcsy contends that, while the ARO 12m Radio Telescope has some similar characteristics, it also differs in several aspects from the subject's description.

Geographic entities mentioned:
surface_form: Kitt Peak
instance_of: Mountain
countries: United States
coordinates: lat: 31.963966666667
lon: -111.59983611111
In a letter to Lyon dated two days before the seal was approved by the convention, Garnett described the landscape as a &quot;view of the Bay of San Francisco and its vessels&quot;, and in 1899, Garnett's brother referred to the mountain as Mount Diablo, supports Robert's view, if Minerva is placed in San Francisco and 'up' is toward the east.

Geographic entities mentioned:
surface_form: Mount Diablo
instance_of: Mountain
countries: United States
coordinates: lat: 37.881697781
lon: -121.914154997
Highland Village Museum/An Clachan Gàidhealach. The Highland Village Museum / Baile nan Gàidheal / An Clachan Gàidhealaich is an outdoor living history museum dedicated to Nova Scotia’s Gaelic folk-life, culture, and language. Highland Village is located in Iona, Nova Scotia, Canada, on 43 acres of natural landscape overlooking the Bras d'Or Lake in Central Cape Breton. History.

Geographic entities mentioned:
surface_form: Bras d'Or Lake
instance_of: Lake
countries: Canada
coordinates: lat: 45.860277777778
lon: -60.778888888889