Sarmila/GeoWiki-Features huggingface dataset:
It meets monthly to implement park planning and improvement and gather citizen input. Within the Boring Lava Field, Mount Tabor and Powell Butte are better known for their recreational uses than other cones. Powell Butte Nature Park offers of trails, with many formal and informal paths. The top of the butte also offers views of Mount Adams, Mount Hood, Mount Jefferson, and Mount St. Helens.

Geographic entities mentioned:
surface_form: Mount Hood
instance_of: Mountain
countries: United States
coordinates: lat: 45.37361111111111
lon: -121.69583333333334
surface_form: Mount St. Helens
instance_of: Mountain
countries: United States
coordinates: lat: 46.200277777778
lon: -122.18944444444
surface_form: mount jefferson
instance_of: Mountain
countries: United States
coordinates: lat: 44.6743006
lon: -121.799573611
surface_form: jefferson
instance_of: Mountain
countries: United States
coordinates: lat: 44.6743006
lon: -121.799573611
surface_form: st. helens
instance_of: Mountain
countries: United States
coordinates: lat: 46.200277777778
lon: -122.18944444444
surface_form: mount jefferson
instance_of: Mountain
countries: United States
coordinates: lat: 45.3522
lon: -68.2828
surface_form: mount jefferson
instance_of: Mountain
countries: United States
coordinates: lat: 42.4584
lon: -74.6196
Powell Butte lies northwest of the Boring Hills, and the surrounding area includes (moving clockwise from the north) other volcanic centers like Green Mountain, Prune Hill, Chamberlain Hill, Devils Rest, Larch Mountain, Pepper Mountain, Kelly Butte, and Mount Tabor.

Geographic entities mentioned:
surface_form: green mountain
instance_of: Mountain
countries: United States
coordinates: lat: 39.9822
lon: -105.302
surface_form: green mountain
instance_of: Mountain
countries: United States
coordinates: lat: 48.291666666667
lon: -121.23861111111
surface_form: kelly butte
instance_of: Mountain
countries: United States
coordinates: lat: 47.169166666667
lon: -121.49027777778
surface_form: powell butte
instance_of: Mountain
countries: United States
coordinates: lat: 45.487347222222
lon: -122.50179722222
Powell Butte. Powell Butte is an extinct cinder cone butte in Portland, Oregon, United States. It is part of the Boring Lava Field, which includes more than 80 small volcanic edifices and lava flows in the Portland–Vancouver metropolitan area. The region around Powell Butte has a cool climate, and the butte and its surroundings feature meadows, rivers, and mixed forests.

Geographic entities mentioned:
surface_form: powell butte
instance_of: Mountain
countries: United States
coordinates: lat: 45.487347222222
lon: -122.50179722222
It is part of the Boring Lava Field, which includes more than 80 small volcanic edifices and lava flows in the Portland–Vancouver metropolitan area. The region around Powell Butte has a cool climate, and the butte and its surroundings feature meadows, rivers, and mixed forests. Powell Butte hosts the Powell Butte Nature Park, which includes about of trails for biking, hiking, and horseback riding.

Geographic entities mentioned:
surface_form: powell butte
instance_of: Mountain
countries: United States
coordinates: lat: 45.487347222222
lon: -122.50179722222
The region around Powell Butte has a cool climate, and the butte and its surroundings feature meadows, rivers, and mixed forests. Powell Butte hosts the Powell Butte Nature Park, which includes about of trails for biking, hiking, and horseback riding. Powell Butte lies within historic territory of the Confederated Tribes of the Grand Ronde Community of Oregon.

Geographic entities mentioned:
surface_form: powell butte
instance_of: Mountain
countries: United States
coordinates: lat: 45.487347222222
lon: -122.50179722222
surface_form: powell butte
instance_of: Mountain
countries: United States
coordinates: lat: 45.487347222222
lon: -122.50179722222
Powell Butte hosts the Powell Butte Nature Park, which includes about of trails for biking, hiking, and horseback riding. Powell Butte lies within historic territory of the Confederated Tribes of the Grand Ronde Community of Oregon. The land surrounding the butte has been used for an orchard and dairy farming.

Geographic entities mentioned:
surface_form: powell butte
instance_of: Mountain
countries: United States
coordinates: lat: 45.487347222222
lon: -122.50179722222
The land surrounding the butte has been used for an orchard and dairy farming. Today two underground reservoirs at the Butte each hold of fresh water as a primary part of the public water system for Portland and much of the surrounding region. Geography and geology. Powell Butte is located in Multnomah County in the U.S. state of Oregon. According to the U.S.

Geographic entities mentioned:
surface_form: powell butte
instance_of: Mountain
countries: United States
coordinates: lat: 45.487347222222
lon: -122.50179722222
J.E. Allen, an emeritus professor of Geology at Portland State University, listed its elevation as in a 1975 publication. Powell Butte is a cinder cone butte and is part of the Plio-Pleistocene Boring Lava Field, a group of volcanic cones that got their name from the low, forested Boring Hills formation.

Geographic entities mentioned:
surface_form: powell butte
instance_of: Mountain
countries: United States
coordinates: lat: 45.487347222222
lon: -122.50179722222
The top of Powell Butte consists of volcanic rock from the Troutdale Formation, on top of which are remnants from a local eruption in the Boring Lava Field, including scoria and volcanic ash. Powell Butte is one of the smaller volcanic cones in the Boring Lava Field.

Geographic entities mentioned:
surface_form: powell butte
instance_of: Mountain
countries: United States
coordinates: lat: 45.487347222222
lon: -122.50179722222
After these hyaloclastite units were deposited, further deformation occurred, leading to the accumulation of gravel and lithic fragments to elevations of in the Portland area. Powell Butte is partially mantled by post hyaloclastite gravel from the Troutdale Formation, which is likely the result of redeposited soil after erosion. Like the rest of the Boring Lava Field, Powell Butte is extinct.

Geographic entities mentioned:
surface_form: powell butte
instance_of: Mountain
countries: United States
coordinates: lat: 45.487347222222
lon: -122.50179722222
Powell Butte is partially mantled by post hyaloclastite gravel from the Troutdale Formation, which is likely the result of redeposited soil after erosion. Like the rest of the Boring Lava Field, Powell Butte is extinct. Climate and ecology. The climate at Powell Butte is cool, creating a short growing season environment. It supports grass meadows, which sustain apple, pear, and walnut trees.

Geographic entities mentioned:
surface_form: powell butte
instance_of: Mountain
countries: United States
coordinates: lat: 45.487347222222
lon: -122.50179722222
Like the rest of the Boring Lava Field, Powell Butte is extinct. Climate and ecology. The climate at Powell Butte is cool, creating a short growing season environment. It supports grass meadows, which sustain apple, pear, and walnut trees. Powell Butte sits near Johnson Creek, a tributary of the Willamette River that sustains native salmon and rainbow trout.

Geographic entities mentioned:
surface_form: powell butte
instance_of: Mountain
countries: United States
coordinates: lat: 45.487347222222
lon: -122.50179722222
Climate and ecology. The climate at Powell Butte is cool, creating a short growing season environment. It supports grass meadows, which sustain apple, pear, and walnut trees. Powell Butte sits near Johnson Creek, a tributary of the Willamette River that sustains native salmon and rainbow trout. It also supports the Powell Butte Nature Park and its associated meadow and forest areas.

Geographic entities mentioned:
surface_form: powell butte
instance_of: Mountain
countries: United States
coordinates: lat: 45.487347222222
lon: -122.50179722222
Powell Butte sits near Johnson Creek, a tributary of the Willamette River that sustains native salmon and rainbow trout. It also supports the Powell Butte Nature Park and its associated meadow and forest areas. These habitats are populated by bats, black-tailed mule deer, chipmunks, coyotes, gray foxes, ground squirrels, rabbits, raccoons, ring-necked pheasants, and skunks.

Geographic entities mentioned:
surface_form: powell butte
instance_of: Mountain
countries: United States
coordinates: lat: 45.487347222222
lon: -122.50179722222
Human history. Powell Butte lies within historic territory of the Confederated Tribes of the Grand Ronde Community of Oregon, which covered more than and extended from the Columbia River to the Klamath River. At the end of the 19th century, much of the meadow area near Powell Butte was cleared and replaced with an orchard by settlers.

Geographic entities mentioned:
surface_form: powell butte
instance_of: Mountain
countries: United States
coordinates: lat: 45.487347222222
lon: -122.50179722222
At the end of the 19th century, much of the meadow area near Powell Butte was cleared and replaced with an orchard by settlers. In 1925, the Portland city government bought the land encompassing Powell Butte from George Wilson with the intent to use it for water reservoirs.

Geographic entities mentioned:
surface_form: powell butte
instance_of: Mountain
countries: United States
coordinates: lat: 45.487347222222
lon: -122.50179722222
They leased the northeastern part of the land to farmer Henry Anderegg, who owned and operated the Meadowland Crest Dairy until 1948. In the mid-1970s, Portland's Water Bureau created a development plan for Powell Butte including four underground reservoirs to be built at the northern side of the mountain. The first of these reservoirs was constructed in 1981 and the second in 2014. Recreation.

Geographic entities mentioned:
surface_form: powell butte
instance_of: Mountain
countries: United States
coordinates: lat: 45.487347222222
lon: -122.50179722222
Recreation. Powell Butte hosts the Powell Butte Nature Park, which encompasses an area of about. The nature park was established by Portland city government in 1987 and opened to the public in 1990 and is maintained by Portland Parks & Recreation; it currently includes a natural area, trails for biking, horseback riding, and hiking.

Geographic entities mentioned:
surface_form: powell butte
instance_of: Mountain
countries: United States
coordinates: lat: 45.487347222222
lon: -122.50179722222
surface_form: powell butte
instance_of: Mountain
countries: United States
coordinates: lat: 45.487347222222
lon: -122.50179722222
The nature park was established by Portland city government in 1987 and opened to the public in 1990 and is maintained by Portland Parks & Recreation; it currently includes a natural area, trails for biking, horseback riding, and hiking. The Friends of Powell Butte is an organization formed in 1990, which is focused on protecting the resources of the nature park.

Geographic entities mentioned:
surface_form: powell butte
instance_of: Mountain
countries: United States
coordinates: lat: 45.487347222222
lon: -122.50179722222
It meets monthly to implement park planning and improvement and gather citizen input. Within the Boring Lava Field, Mount Tabor and Powell Butte are better known for their recreational uses than other cones. Powell Butte Nature Park offers of trails, with many formal and informal paths. The top of the butte also offers views of Mount Adams, Mount Hood, Mount Jefferson, and Mount St. Helens.

Geographic entities mentioned:
surface_form: powell butte
instance_of: Mountain
countries: United States
coordinates: lat: 45.487347222222
lon: -122.50179722222
Guise herself became regent in 1554. On 5 August 1557, Moray, his half-brother Lord Robert, and Lord Home led a raiding party from Edinburgh towards Ford Castle in Northumberland and burnt houses at Fenton and in Glendale, before retreating on the approach of an English force led by Henry Percy, 8th Earl of Northumberland.

Geographic entities mentioned:
surface_form: Glendale
instance_of: Valley
countries: United Kingdom
coordinates: lat: 55.595083
lon: -2.105
At Inverness, on 4 June 1569, Moray met the Highland and Island chiefs with the Earls of Caithness and Sutherland and Lord Lovat. His secretary, John Wood, said &quot;such a power had seldom been seen there,&quot; Moray wrote that &quot;the journey is to put down troubles in the north.&quot;
In March 1569 Moray came from Kelso to Liddesdale and spoke to the English border warden, Sir John Forster.

Geographic entities mentioned:
surface_form: Liddesdale
instance_of: Valley
countries: United Kingdom
coordinates: lat: 55.2
lon: -2.75
Puerto Rico Highway 577. Puerto Rico Highway 577 (PR-577) is a short tertiary mountainous state road that connects PR-143 (also known as &quot;Ruta Panorámica&quot; [Scenic Route] in this sector) to the Cerro Maravilla communications towers, in Barrio Anón, Ponce, Puerto Rico.

Geographic entities mentioned:
surface_form: Cerro Maravilla
instance_of: Mountain
countries: United States
coordinates: lat: 18.1531
lon: -66.5542
Situated at an elevation of, Taebaek is the second highest city in South Korea, after Pyeongchang. Etymology. Taebaek in is derived from Taebaeksan, meaning &quot;very bright.&quot;
Attractions. Manggyeongsa Temple in Hyeol-dong, at an elevation of 1,460 meters on the Taebaek Mountains, is a temple built to enshrine the statue of the Bodhisattva of wisdom.

Geographic entities mentioned:
surface_form: Taebaeksan
instance_of: Mountain
countries: South Korea
coordinates: lat: 37.095730555556
lon: 128.91523888889
Distribution and habitat. The lily-of-the-valley orchid grows on trees, rocks and cliffs and on well-lit upper branches of rainforest trees between the Atherton Tableland in Queensland and Grafton in New South Wales.

Geographic entities mentioned:
surface_form: Atherton Tableland
instance_of: Plateau
countries: Australia
coordinates: lat: -17.16666667
lon: 145.53333333
The igneous activity of the Karoo LIP began at the northern margin of the province. The long-lasting Chon-Aike Province in Patagonia, the Antarctic Peninsula, and Ellsworth Land was activated in an unstable tectonic environment in which both extension and subduction occurred. Chon-Aike had a peak between but produced continued magmatism between.

Geographic entities mentioned:
surface_form: Ellsworth Land
instance_of: Plateau
coordinates: lat: -75.5
lon: -80
Dawa Thondup. Dawa Thondup (1907-1973) (also Da Thondup, Dawa Tendrup or Da Thundu) was a Sherpa mountaineer from the Nepali village of Khumjung. He had been a porter on the 1933 British Mount Everest expedition, he survived the 1934 Nanga Parbat climbing disaster, and he was a team member on a 1935 expedition led by James Waller and John Hunt to Saltoro Kangri.

Geographic entities mentioned:
surface_form: Saltoro Kangri
instance_of: Mountain
countries: Pakistan
coordinates: lat: 35.399578333333
lon: 76.847516666667
He had been a porter on the 1933 British Mount Everest expedition, he survived the 1934 Nanga Parbat climbing disaster, and he was a team member on a 1935 expedition led by James Waller and John Hunt to Saltoro Kangri. In 1937, he was with Hunt again during an expedition in the Kanchenjunga area. The next year, he was part of a group led by James Waller that attempted to climb Masherbrum.

Geographic entities mentioned:
surface_form: Masherbrum
instance_of: Mountain
countries: Pakistan
coordinates: lat: 35.6425
lon: 76.310833333333
Thondup participated in the disastrous 1939 American Karakoram expedition to K2. He may have been part of the English-Swiss expedition in 1950 that was the first to summit Abi Gamin. and was a porter on the Swiss expedition to Everest in 1952. He also participated in 1953 British Mount Everest expedition led by Col. John Hunt.

Geographic entities mentioned:
surface_form: Abi Gamin
instance_of: Mountain
countries: India
coordinates: lat: 30.93
lon: 79.6
She described the relationship by saying they were soulmates. He died in 1981; by the following year, Powers was founding President of the William Holden Wildlife Foundation and a director of the Mount Kenya Game Ranch and Wildlife Conservancy in Nanyuki, Kenya. In the United States, she works with both the Cincinnati Zoo and Atlanta Zoo.

Geographic entities mentioned:
surface_form: Mount Kenya
instance_of: Mountain
countries: Kenya
coordinates: lat: -0.1
lon: 37.2
Lakeridge, West Hill. Lakeridge is a hillside neighborhood near Lake Washington located mostly in unincorporated West Hill in King County, Washington, and partially in the City of Seattle. Its boundaries extend from Seattle's Rainier Beach neighborhood on the north, to Lake Washington on the east, to unincorporated Bryn Mawr on the southeast and unincorporated Skyway on the southwest.

Geographic entities mentioned:
surface_form: Lake Washington
instance_of: Lake
countries: United States
coordinates: lat: 47.616666666667
lon: -122.26472222222
Lakeridge is a hillside neighborhood near Lake Washington located mostly in unincorporated West Hill in King County, Washington, and partially in the City of Seattle. Its boundaries extend from Seattle's Rainier Beach neighborhood on the north, to Lake Washington on the east, to unincorporated Bryn Mawr on the southeast and unincorporated Skyway on the southwest. History and plats.

Geographic entities mentioned:
surface_form: Lake Washington
instance_of: Lake
countries: United States
coordinates: lat: 47.616666666667
lon: -122.26472222222
Some is made into sparkling wine in the far northeast around Poysdorf. Along the Danube to the west of Vienna, in Wachau, Kremstal and Kamptal, it grows with Riesling in terraces on slopes so steep they can barely retain any soil. The result is a very pure, mineral wine capable of long aging, that stands comparison with some of the great wines of the world.

Geographic entities mentioned:
surface_form: Kremstal
instance_of: Valley
countries: Austria
The grape is authorized in five &quot;Districtus Austriae Controllatus&quot; (DAC) regions—the Weinviertel where it is the only permitted grape variety; Leithaberg where it can be made as a varietal or blended with Pinot blanc, Chardonnay and Neuburger; Traisental, Kremstal and Kamptal where it is planted with Riesling.

Geographic entities mentioned:
surface_form: Kremstal
instance_of: Valley
countries: Austria
There is of Grüner Veltliner planted in Hungary where the grape is known as &quot;Zöld Veltlini&quot;. The majority of these plantings are found in the western wine regions around Lake Balaton, the northern vineyards in the foothills of the Mátra mountains and the southern wine regions of Tolna County and Kunság. Some plantings of Grüner Veltliner can also be found in Bulgaria. In the New World.

Geographic entities mentioned:
surface_form: Lake Balaton
instance_of: Lake
countries: Hungary
coordinates: lat: 46.85
lon: 17.72
Other notable Oregon Growers include Chehalem Winery, Raptor Ridge Winery, and Illahe Vineyards. New York State's Finger Lakes AVA is home to some small plantings of Grüner Veltliner due to the cool climate and proximity to the glacially formed Finger Lakes which help mitigate excessive cold in the early spring and the winter.

Geographic entities mentioned:
surface_form: Finger Lakes
instance_of: Group of lakes
countries: United States
coordinates: lat: 42.666666666667
lon: -76.833333333333
The view is blocked by a great rock protruding from the middle of the upper fall, so that the whole waterfall can be seen clearly only from the bottom. The Hayato Great Falls is located deep within Tanzawa Mountains, and is accessible only by a two-hour hike on poorly marked and maintained mountain trails from the nearest road.

Geographic entities mentioned:
surface_form: Tanzawa Mountains
instance_of: Mountain
countries: Japan
coordinates: lat: 35.474166666667
lon: 139.16277777778
The Osings in the Banyuwangi Regency of East Java are a community whose religion shows many similarities to that of Bali. The Tenggerese communities at the foot of Mount Bromo are officially Hindu, but their religion includes many elements of Buddhism including the worship of Lord Buddha along with Hindu trinity Shiva, Vishnu, and Brahma.

Geographic entities mentioned:
surface_form: Mount Bromo
instance_of: Mountain
countries: Indonesia
coordinates: lat: -7.9430555555556
lon: 112.95388888889
Westbury Brook Ironstone Mine () is a biological Site of Special Scientific Interest in Gloucestershire, notified in 1998. Location and habitat. The mine is one of a series of Sites of Special Scientific Interest within the Forest of Dean and Wye Valley (Gloucestershire and Monmouthshire). These sites support (between them) breeding and hibernation roosts for Lesser and Greater horseshoe bats.

Geographic entities mentioned:
surface_form: Wye Valley
instance_of: Valley
countries: United Kingdom
coordinates: lat: 51.69255
lon: -2.66283
Jebel Proywe. Jebel Proywe is a mountain in the Abarim range in Jordan. Its peak is above sea level. It is around north of Triclinium the ancient Nabataean ruins known also as Little Petra and south-west of Shobak.

Geographic entities mentioned:
surface_form: jebel proywe
instance_of: Mountain
countries: Jordan
coordinates: lat: 30.451944
lon: 35.440556
Mount Manning. Mount Manning is a mountain located in New South Wales, Australia.

Geographic entities mentioned:
surface_form: mount manning
instance_of: Mountain
countries: Australia
coordinates: lat: -33.1167
lon: 151.1
Cerro Tenerife (Chile). Cerro Tenerife is a mountain located next to the small town of Puerto Natales and Torres del Paine National Park in Chilean Patagonia.

Geographic entities mentioned:
surface_form: cerro tenerife
instance_of: Mountain
countries: Chile
coordinates: lat: -51.38333333
lon: -72.95
Early life. Lucretia Louise del Valle was born in Los Angeles, California, the daughter of Reginaldo Francisco del Valle and Helen May White del Valle. Her father, a California state senator, owned Rancho Camulos. Her grandparents Ygnacio del Valle and Ysabel del Valle owned much of the Santa Clarita Valley. Career.

Geographic entities mentioned:
surface_form: Santa Clarita Valley
instance_of: Valley
countries: United States
coordinates: lat: 34.398
lon: -118.522
2003 Sri Lanka cyclone. The 2003 Sri Lanka cyclone was a moderately powerful tropical cyclone that produced the worst flooding in Sri Lanka in 56 years. The first storm of the 2003 North Indian Ocean cyclone season, it developed over the Bay of Bengal on May 10. Favorable environmental conditions allowed the system to intensify steadily while moving northwestward.

Geographic entities mentioned:
surface_form: Bay of Bengal
instance_of: Body of water
countries: India
Bangladesh
Sri Lanka
Myanmar
coordinates: lat: 15
lon: 88
On the way to the Heavenly Lake near Urumqi in China are a pair of trees that local people have called the Husband and Wife trees because they are connected by a living branch. The Tatajia Husband and Wife trees are in Taiwan and in Yakushima, Kagoshima-ken, Japan, are a pair of Husband and Wife trees formed from conjoined cedars. In Lambeg, Co.

Geographic entities mentioned:
surface_form: Heavenly Lake
instance_of: Lake
countries: People's Republic of China
coordinates: lat: 43.885833333333
lon: 88.1325
Ossimo. Ossimo (Camunian:) is a town and &quot;comune&quot; in the province of Brescia, Lombardy, northern Italy. It is part of Val Camonica, and is divided into two centers: Ossimo Superiore and Ossimo Inferiore. It can be reached by the provincial road 5, that leads from Malegno to Borno.

Geographic entities mentioned:
surface_form: Val Camonica
instance_of: Valley
countries: Italy
coordinates: lat: 46.0075
lon: 10.3475
The Anna River is a river on the Upper Peninsula of the U.S. state of Michigan. The mouth of the river is at in the city of Munising on the South Bay of Grand Island Harbor on Lake Superior. The river rises in the Anna Marsh in eastern Au Train Township at. It flows first to the southeast, then turns mostly east and receives the outflow from Mud Lake and the Valley Spur Creek.

Geographic entities mentioned:
surface_form: Lake Superior
instance_of: Lake
countries: Canada
United States
coordinates: lat: 47.52881611111111
lon: -87.76002194444445
The largest lagoon along the North American East Coast, it extends long and wide. It is part of a large, interconnected network of similar lagoons that includes Albemarle Sound, Currituck Sound, Croatan Sound, Roanoke Sound, Pamlico Sound, Bogue Sound, Back Sound, and Core Sound known collectively as the Albemarle-Pamlico sound system. With over 3,000 sq. mi.

Geographic entities mentioned:
surface_form: Croatan Sound
instance_of: Landform
countries: United States
coordinates: lat: 35.8375
lon: -75.69722222
surface_form: Roanoke Sound
instance_of: Landform
countries: United States
coordinates: lat: 35.86333333
lon: -75.60861111
surface_form: Back Sound
instance_of: Landform
countries: United States
coordinates: lat: 34.68472222
lon: -76.57055556
surface_form: Core Sound
instance_of: Landform
countries: United States
coordinates: lat: 34.85222222
lon: -76.34833333
The Albemarle-Pamlico Sound is one of nineteen great waters recognized by the America's Great Waters Coalition. Hydrology. Pamlico Sound is connected to the north with Albemarle Sound through passages provided by the Roanoke Sound and Croatan Sound. Core Sound is located at the Pamlico's narrow southern end.

Geographic entities mentioned:
surface_form: Roanoke Sound
instance_of: Landform
countries: United States
coordinates: lat: 35.86333333
lon: -75.60861111
surface_form: Croatan Sound
instance_of: Landform
countries: United States
coordinates: lat: 35.8375
lon: -75.69722222
The Albemarle-Pamlico Sound is one of nineteen great waters recognized by the America's Great Waters Coalition. Hydrology. Pamlico Sound is connected to the north with Albemarle Sound through passages provided by the Roanoke Sound and Croatan Sound. Core Sound is located at the Pamlico's narrow southern end.

Geographic entities mentioned:
surface_form: Core Sound
instance_of: Landform
countries: United States
coordinates: lat: 34.85222222
lon: -76.34833333
Core Sound is located at the Pamlico's narrow southern end. It is fed by the Neuse and Pamlico rivers (the latter of which is the estuary of the Tar River) from the west, and from the east by Oregon Inlet, Hatteras Inlet, and Ocracoke Inlet, which also provide passage to the Atlantic Ocean.

Geographic entities mentioned:
surface_form: Oregon Inlet
instance_of: Landform
countries: United States
coordinates: lat: 35.77463889
lon: -75.53136111
The book illustrated the plight of the Japanese people and the impact of an earthquake on their environment, in dramatic images that were printed by Ogawa Kazumasa
In addition to photographing the 1891 Mino–Owari earthquake, Burton also photographed Japanese costumes and customs, Hakone, Mount Fuji, and scenes from daily life.

Geographic entities mentioned:
surface_form: Mount Fuji
instance_of: Mountain
countries: Japan
coordinates: lat: 35.36055555555556
lon: 138.7275
Auwers (crater). Auwers is a small lunar impact crater located in the Montes Haemus mountain range at the south edge of Mare Serenitatis. It is named after German astronomer Arthur Auwers. It lies southeast of the crater Menelaus. The irregular rim of Auwers has a gap at the north-northwest edge, which allowed lava flows to reach the crater floor and flood the interior. Satellite craters.

Geographic entities mentioned:
surface_form: Montes Haemus
instance_of: Mountain
coordinates: lat: 17.11
lon: 12.03
He did not seek a second term in office. After his term, in 1868, he was appointed to the Board of Water Commissioners and oversaw construction of the water inlet pier in the Niagara River. In 1870, Wells began importing sand for paving and building purposes from property purchased at Point Abino on Lake Erie. Personal life. On April 20, 1837, he married Susan Jane Wheeler.

Geographic entities mentioned:
surface_form: Lake Erie
instance_of: Lake
countries: Canada
United States
coordinates: lat: 42.25
lon: -80.99972222222222
Mount Claywood. Mount Claywood is a mountain summit located within Olympic National Park in Jefferson County of Washington state. It is situated at the head of Lost River, and 15 mi (24 km) east of Mount Olympus. Its nearest higher neighbor is Mount Cameron, to the northeast. Other nearby peaks include Mt. Fromme, to the southeast, and Sentinel Peak, also to the southeast.

Geographic entities mentioned:
surface_form: jefferson
instance_of: Mountain
countries: United States
coordinates: lat: 44.6743006
lon: -121.799573611
surface_form: washington
instance_of: Lake
countries: United States
coordinates: lat: 47.616666666667
lon: -122.26472222222
surface_form: a mountain
instance_of: Mountain
countries: United States
coordinates: lat: 32.2925
lon: -106.69777777778
surface_form: mount claywood
instance_of: Mountain
countries: United States
coordinates: lat: 47.80065
lon: -123.3699
It is situated at the head of Lost River, and 15 mi (24 km) east of Mount Olympus. Its nearest higher neighbor is Mount Cameron, to the northeast. Other nearby peaks include Mt. Fromme, to the southeast, and Sentinel Peak, also to the southeast. Precipitation runoff from the mountain drains north and west into tributaries of the Elwha River, and east into Claywood Lake, thence Dosewallips River.

Geographic entities mentioned:
surface_form: sentinel peak
instance_of: Mountain
countries: United States
coordinates: lat: 36.0158
lon: -118.527
surface_form: sentinel peak
instance_of: Mountain
countries: United States
coordinates: lat: 48.3562
lon: -121.041
surface_form: sentinel peak
instance_of: Mountain
countries: United States
coordinates: lat: 58.99277777777778
lon: -136.5625
surface_form: sentinel peak
instance_of: Mountain
countries: United States
coordinates: lat: 32.2106
lon: -110.992
surface_form: sentinel peak
instance_of: Mountain
countries: United States
coordinates: lat: 36.096666
lon: -117.077657
surface_form: sentinel peak
instance_of: Mountain
countries: United States
coordinates: lat: 47.77842
lon: -123.34268
Mount Claywood. Mount Claywood is a mountain summit located within Olympic National Park in Jefferson County of Washington state. It is situated at the head of Lost River, and 15 mi (24 km) east of Mount Olympus. Its nearest higher neighbor is Mount Cameron, to the northeast. Other nearby peaks include Mt. Fromme, to the southeast, and Sentinel Peak, also to the southeast.

Geographic entities mentioned:
surface_form: mount cameron
instance_of: Mountain
countries: United States
coordinates: lat: 47.82537
lon: -123.32851
surface_form: mount cameron
instance_of: Mountain
countries: United States
coordinates: lat: 39.34693
lon: -106.11863
surface_form: mount cameron
instance_of: Mountain
countries: United States
coordinates: lat: 61.21
lon: -146.665
Mount Claywood. Mount Claywood is a mountain summit located within Olympic National Park in Jefferson County of Washington state. It is situated at the head of Lost River, and 15 mi (24 km) east of Mount Olympus. Its nearest higher neighbor is Mount Cameron, to the northeast. Other nearby peaks include Mt. Fromme, to the southeast, and Sentinel Peak, also to the southeast.

Geographic entities mentioned:
surface_form: mount olympus
instance_of: Mountain
countries: United States
coordinates: lat: 47.801305555556
lon: -123.71083333333
surface_form: mount olympus
instance_of: Mountain
countries: United States
coordinates: lat: 40.6566
lon: -111.771
Mount Claywood. Mount Claywood is a mountain summit located within Olympic National Park in Jefferson County of Washington state. It is situated at the head of Lost River, and 15 mi (24 km) east of Mount Olympus. Its nearest higher neighbor is Mount Cameron, to the northeast. Other nearby peaks include Mt. Fromme, to the southeast, and Sentinel Peak, also to the southeast.

Geographic entities mentioned:
surface_form: mount claywood
instance_of: Mountain
countries: United States
coordinates: lat: 47.80065
lon: -123.3699
Mt. Claywood marks the expedition's deepest penetration from the north into the Olympic wilderness. Climate. Based on the Köppen climate classification, Mount Claywood is located in the marine west coast climate zone of western North America. Weather fronts originating in the Pacific Ocean travel northeast toward the Olympic Mountains.

Geographic entities mentioned:
surface_form: mount claywood
instance_of: Mountain
countries: United States
coordinates: lat: 47.80065
lon: -123.3699
History. This mountain was originally named &quot;Mount Clay Wood&quot; in 1885 by Lieutenant Joseph P. O'Neil to honor his superior, Colonel Henry Clay Wood (1832–1918), Assistant Adjutant General, Department of the Columbia, who signed the orders for O'Neil's 1885 exploration of the Olympic Mountains. Mt.

Geographic entities mentioned:
surface_form: mount clay wood
instance_of: Mountain
countries: United States
coordinates: lat: 47.80065
lon: -123.3699
surface_form: mount clay
instance_of: Mountain
countries: United States
coordinates: lat: 44.285166666667
lon: -71.315833333333
Creag Ghuanach. Creag Ghuanach (621 m) is a mountain in the Grampian Mountains of Scotland. It is located in Lochaber, at the southern head of Loch Treig. A small but very craggy peak, Creag Ghuanach rises steeply from the loch below. The nearest village is Roybridge several miles to the north.

Geographic entities mentioned:
surface_form: Loch Treig
instance_of: Lake
countries: United Kingdom
coordinates: lat: 56.81399
lon: -4.72704
Creag Ghuanach. Creag Ghuanach (621 m) is a mountain in the Grampian Mountains of Scotland. It is located in Lochaber, at the southern head of Loch Treig. A small but very craggy peak, Creag Ghuanach rises steeply from the loch below. The nearest village is Roybridge several miles to the north.

Geographic entities mentioned:
surface_form: creag ghuanach
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 56.781399
lon: -4.785769
It rises approximately along its northern base from the Middle Prong of the Little Pigeon River, also known as Greenbrier Creek. On August 12, 1944, a Beechcraft Model 17 Staggerwing from Oak Ridge, Tennessee, crashed into Woolly Tops Mountain. The wreckage was not discovered until January 19, 1947, by a group of hikers from the Smoky Mountain Hiking Club.

Geographic entities mentioned:
surface_form: oak ridge
instance_of: Landform
countries: United States
coordinates: lat: 37.46
lon: -121.722
surface_form: woolly tops mountain
instance_of: Mountain
countries: United States
coordinates: lat: 35.67704
lon: -83.3396
Woolly Tops Mountain. Woolly Tops Mountain is a mountain in the Great Smoky Mountains in Sevier County, Tennessee. It has an elevation of, and is located in the eastern half of the Great Smoky Mountains National Park. Description. Woolly Tops Mountain is a large massif oriented in an east–west direction, which reaches a maximum elevation of.

Geographic entities mentioned:
surface_form: woolly tops mountain
instance_of: Mountain
countries: United States
coordinates: lat: 35.67704
lon: -83.3396
It has an elevation of, and is located in the eastern half of the Great Smoky Mountains National Park. Description. Woolly Tops Mountain is a large massif oriented in an east–west direction, which reaches a maximum elevation of. It is located approximately north of Laurel Top on the Tennessee-North Carolina state line.

Geographic entities mentioned:
surface_form: woolly tops mountain
instance_of: Mountain
countries: United States
coordinates: lat: 35.67704
lon: -83.3396
Gray-footed chipmunk. The gray-footed chipmunk (&quot;Neotamias canipes&quot;) is a terrestrial and forest-dwelling species of chipmunk and rodent in the family Sciuridae. It is endemic to New Mexico and in the Sierra Diablo and Guadalupe Mountains in the Trans-Pecos region of Texas in the United States. Its natural habitat are coniferous forests.

Geographic entities mentioned:
surface_form: Trans-Pecos
instance_of: Valley
countries: United States
coordinates: lat: 30.56
lon: -103.79
The chipmunk has a karyotype of &quot;A&quot;. Distribution and habitat. Gray-footed chipmunks are native to the southeastern mountain ranges of New Mexico such as the Sacramento, Gallinas, and Jicarilla. They are also to mountain ranges in Texas such as the Guadalupe in the Trans-Pecos region. The chipmunks are found primarily at elevations of, but have been recorded at lower elevations.

Geographic entities mentioned:
surface_form: Trans-Pecos region
instance_of: Valley
countries: United States
coordinates: lat: 30.56
lon: -103.79
Clough River. The Clough River is a river in Cumbria, England. A tributary of the River Rawthey, it flows for primarily through the Garsdale valley. Course. The river rises at Grisedale in south-eastern Cumbria, where a group of smaller streams draining Grisedale Pike converge as Grisedale Beck.

Geographic entities mentioned:
surface_form: Garsdale
instance_of: Valley
countries: United Kingdom
coordinates: lat: 54.301
lon: -2.391
The young Clough River then goes through a short valley (Grisedale, &quot;The Dale That Died&quot;), and over a waterfall before being named Clough at Clough Farm, Garsdale Head, where it enters Garsdale, a valley formed by the river between Baugh Fell (to the north) and Rise Hill (to the south).

Geographic entities mentioned:
surface_form: Grisedale
instance_of: Valley
countries: United Kingdom
coordinates: lat: 54.333333333333
lon: -2.35
surface_form: Garsdale
instance_of: Valley
countries: United Kingdom
coordinates: lat: 54.301
lon: -2.391
Additionally, Babol is the first northern city in Iran to establish a national medical university. The city is located between the Caspian Sea and the Alborz mountain range, 178 kilometers northeast of Tehran (the capital of Iran). History and etymology.

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
It is famous for its orange groves. Location. Babol is in the north of Iran, north-east of Tehran, between the northern slopes of the Alborz Mountains and southern coast of the Caspian Sea.The city is located approximately 20 kilometers south of the Caspian Sea on the west bank of Babolrud River.

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
Eotypotherium. &quot;Eotypotherium&quot; is an extinct genus of mammal, belonging to the suborder Typotheria. It lived during the Early Miocene. Its fossilized remains were discovered in the Chucal Formation, in the Chilean altiplano, near the Salar de Surire, in South America. Etymology.

Geographic entities mentioned:
surface_form: altiplano
instance_of: Plateau
countries: Bolivia
Peru
Chile
Argentina
coordinates: lat: -16.00358
lon: -69.65332
The Metacomet Ridge extends north from West Rock Ridge as Mad Mare Hill and Mount Sanford and northeast as Rocky Top and Sleeping Giant. East of West Rock Ridge, the Metacomet Ridge spreads out into a series of low, parallel ridges toward Saltonstall Mountain in Branford, Connecticut; the only noteworthy summit in between is East Rock which looms over New Haven from the north.

Geographic entities mentioned:
surface_form: Saltonstall Mountain
instance_of: Mountain
countries: United States
coordinates: lat: 41.324
lon: -72.8
surface_form: East Rock
instance_of: Mountain
countries: United States
coordinates: lat: 41.327222222222
lon: -72.904722222222
surface_form: east rock
instance_of: Mountain
countries: United States
coordinates: lat: 41.327222222222
lon: -72.904722222222
surface_form: west rock ridge
instance_of: Mountain
countries: United States
coordinates: lat: 41.380841666667
lon: -72.978319444444
surface_form: saltonstall mountain
instance_of: Mountain
countries: United States
coordinates: lat: 41.324
lon: -72.8
Trails on the property link up with the Regicides Trail on the ridge. The towns of Bethany,
Hamden, and Woodbridge are also invested in the conservation of West Rock Ridge and its viewshed. Adjacent summits. Nearby summits include Mount Sanford to the north, Sleeping Giant to the northeast and East Rock to the east.

Geographic entities mentioned:
surface_form: East Rock
instance_of: Mountain
countries: United States
coordinates: lat: 41.327222222222
lon: -72.904722222222
surface_form: east rock
instance_of: Mountain
countries: United States
coordinates: lat: 41.327222222222
lon: -72.904722222222
surface_form: sleeping giant
instance_of: Mountain
countries: United States
coordinates: lat: 41.430636
lon: -72.890767
surface_form: sleeping giant
instance_of: Landform
countries: United States
coordinates: lat: 22.0608
lon: -159.355
The 5.6 mile long Baldwin Drive heads north from Regicide Drive, ending at West Shepard Avenue in Hamden. Several communications towers sprout from the ridge crest. The Metacomet Ridge extends north from West Rock Ridge as Mad Mare Hill and Mount Sanford and northeast as Rocky Top and Sleeping Giant.

Geographic entities mentioned:
surface_form: sanford
instance_of: Mountain
countries: United States
coordinates: lat: 62.213888888889
lon: -144.12888888889
surface_form: mount sanford
instance_of: Mountain
countries: United States
coordinates: lat: 62.213888888889
lon: -144.12888888889
surface_form: west rock ridge
instance_of: Mountain
countries: United States
coordinates: lat: 41.380841666667
lon: -72.978319444444
surface_form: west rock ridge
instance_of: Mountain
countries: United States
coordinates: lat: 41.380841666667
lon: -72.978319444444
surface_form: rocky top
instance_of: Mountain
countries: United States
coordinates: lat: 34.982222222222
lon: -84.003611111111
surface_form: sleeping giant
instance_of: Mountain
countries: United States
coordinates: lat: 41.430636
lon: -72.890767
surface_form: mount sanford
instance_of: Mountain
countries: United States
coordinates: lat: 41.4617
lon: -72.9486
surface_form: rock ridge
instance_of: Lake
countries: United States
coordinates: lat: 40.9129
lon: -74.4639
surface_form: rock ridge
instance_of: Lake
countries: United States
coordinates: lat: 40.9129
lon: -74.4639
surface_form: sleeping giant
instance_of: Landform
countries: United States
coordinates: lat: 22.0608
lon: -159.355
The ridge boasts a substantial network of hiking trails and park roads, cliffs, rugged woodlands, scenic ponds and reservoirs, and waterfalls. Two noteworthy hiking trails cross the ridge: the Regicides Trail which traverses the summit crest from end to end, and the Quinnipiac Trail which crosses the northern summit of the ridge and extends north over Sanford Mountain and east over Sleeping Giant.

Geographic entities mentioned:
surface_form: sanford
instance_of: Mountain
countries: United States
coordinates: lat: 62.213888888889
lon: -144.12888888889
surface_form: sleeping giant
instance_of: Mountain
countries: United States
coordinates: lat: 41.430636
lon: -72.890767
surface_form: sleeping giant
instance_of: Landform
countries: United States
coordinates: lat: 22.0608
lon: -159.355
West Rock Ridge. West Rock Ridge or West Rock of south-central Connecticut, is a long trap rock mountain ridge located on the west side of New Haven with a high point of at High Rock, also known as York Mountain. The ridge forms a continuous line of exposed cliffs visible from metropolitan New Haven and points west.

Geographic entities mentioned:
surface_form: west rock ridge
instance_of: Mountain
countries: United States
coordinates: lat: 41.380841666667
lon: -72.978319444444
surface_form: rock ridge
instance_of: Lake
countries: United States
coordinates: lat: 40.9129
lon: -74.4639
West Rock Ridge. West Rock Ridge or West Rock of south-central Connecticut, is a long trap rock mountain ridge located on the west side of New Haven with a high point of at High Rock, also known as York Mountain. The ridge forms a continuous line of exposed cliffs visible from metropolitan New Haven and points west.

Geographic entities mentioned:
surface_form: west rock ridge
instance_of: Mountain
countries: United States
coordinates: lat: 41.380841666667
lon: -72.978319444444
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: rock mountain
instance_of: Mountain
countries: United States
coordinates: lat: 47.799444444444
lon: -120.97444444444
surface_form: high rock
instance_of: Mountain
countries: United States
coordinates: lat: 46.684444444444445
lon: -121.90138888888889
surface_form: rock ridge
instance_of: Lake
countries: United States
coordinates: lat: 40.9129
lon: -74.4639
surface_form: high rock
instance_of: Mountain
countries: United States
coordinates: lat: 39.695
lon: -77.5225
The ridge forms a continuous line of exposed cliffs visible from metropolitan New Haven and points west. West Rock Ridge is part of the narrow, linear Metacomet Ridge which extends from Long Island Sound near New Haven north through the Connecticut River Valley of Massachusetts to the Vermont border.

Geographic entities mentioned:
surface_form: west rock ridge
instance_of: Mountain
countries: United States
coordinates: lat: 41.380841666667
lon: -72.978319444444
surface_form: long island
instance_of: Landform
countries: United States
coordinates: lat: 46.7269
lon: -90.785
surface_form: rock ridge
instance_of: Lake
countries: United States
coordinates: lat: 40.9129
lon: -74.4639
surface_form: river valley
instance_of: Valley
countries: United States
coordinates: lat: 35.36
lon: -93.37
West Rock Ridge is part of the narrow, linear Metacomet Ridge which extends from Long Island Sound near New Haven north through the Connecticut River Valley of Massachusetts to the Vermont border. West Rock Ridge is popular for recreation and known for its microclimate ecosystems, rare plant communities, and expansive views from cliffs that tower up to above the surrounding landscape.

Geographic entities mentioned:
surface_form: west rock ridge
instance_of: Mountain
countries: United States
coordinates: lat: 41.380841666667
lon: -72.978319444444
surface_form: rock ridge
instance_of: Lake
countries: United States
coordinates: lat: 40.9129
lon: -74.4639
This act gives the DEEP the right of first refusal to purchase private land within the West Rock Ridge conservation area and to permit increasing the size of the park, which is about. Geography. West Rock Ridge, located in the Connecticut municipalities of New Haven, Hamden, Woodbridge, and Bethany, is wide at its widest point.

Geographic entities mentioned:
surface_form: west rock ridge
instance_of: Mountain
countries: United States
coordinates: lat: 41.380841666667
lon: -72.978319444444
surface_form: rock ridge
instance_of: Lake
countries: United States
coordinates: lat: 40.9129
lon: -74.4639
Judges Cave is also located near the southern end of the ridge. West Rock Ridge is an important aquifer. The ridge is bordered on the west by property owned by the South Central Connecticut Regional Water Authority; reservoirs include Lake Dawson and Lake Watrous. Konolds Pond, which is not used as a water source, is located just north of Rt. 15 in an industrial area.

Geographic entities mentioned:
surface_form: west rock ridge
instance_of: Mountain
countries: United States
coordinates: lat: 41.380841666667
lon: -72.978319444444
surface_form: rock ridge
instance_of: Lake
countries: United States
coordinates: lat: 40.9129
lon: -74.4639
Geology. The fault-block ridge of West Rock is composed of diabase (sometimes referred to as trap rock), an intrusive volcanic rock. Diabase is a dark colored rock, but the iron within it weathers to a rusty brown when exposed to the air, lending the ledges of West Rock Ridge a distinct reddish hue.

Geographic entities mentioned:
surface_form: west rock ridge
instance_of: Mountain
countries: United States
coordinates: lat: 41.380841666667
lon: -72.978319444444
surface_form: rock ridge
instance_of: Lake
countries: United States
coordinates: lat: 40.9129
lon: -74.4639