Sarmila/GeoWiki-Features huggingface dataset:
The summit, located within the University of Massachusetts Amherst's Cadwell Memorial Forest, is traversed by the Metacomet-Monadnock Trail and is the home of the Five Colleges radio station beacon. The west side of Mount Lincoln drains into Hop Brook and Amethyst Brook, thence into Fort River, the Connecticut River, and Long Island Sound.

Geographic entities mentioned:
surface_form: mount lincoln
instance_of: Mountain
countries: United States
coordinates: lat: 44.149
lon: -71.6445
surface_form: mount lincoln
instance_of: Mountain
countries: United States
coordinates: lat: 47.55009
lon: -123.32822
surface_form: long island
instance_of: Landform
countries: United States
coordinates: lat: 46.7269
lon: -90.785
surface_form: mount lincoln
instance_of: Mountain
countries: United States
coordinates: lat: 39.35138889
lon: -106.11083333
surface_form: mount lincoln
instance_of: Mountain
countries: United States
coordinates: lat: 39.28768
lon: -120.32798
surface_form: mount lincoln
instance_of: Mountain
countries: United States
coordinates: lat: 42.3639
lon: -72.4231
The University currently uses the forest to conduct silviculture and ecosystem research. Recreation. The Metacomet-Monadnock Trail traverses over the summit of Mt. Lincoln. Because this section, #11, of the M&M Trail is not entirely on public land, re-routing of the trail because of private ownership issues remains a concern.

Geographic entities mentioned:
surface_form: mt. lincoln
instance_of: Mountain
countries: United States
coordinates: lat: 44.149
lon: -71.6445
surface_form: mt. lincoln
instance_of: Mountain
countries: United States
coordinates: lat: 47.55009
lon: -123.32822
surface_form: mt. lincoln
instance_of: Mountain
countries: United States
coordinates: lat: 39.35138889
lon: -106.11083333
surface_form: mt. lincoln
instance_of: Mountain
countries: United States
coordinates: lat: 39.28768
lon: -120.32798
surface_form: mt. lincoln
instance_of: Mountain
countries: United States
coordinates: lat: 42.3639
lon: -72.4231
The Jabish Canal flows into Broad Brook, thence into the Chicopee River, the Connecticut River, and Long Island Sound; Jabish Brook flows into the Swift River, the Ware River, thence the Chicopee River, Connecticut River, and Long Island Sound. Cadwell Memorial Forest. The forest is named after Frank A.

Geographic entities mentioned:
surface_form: long island
instance_of: Landform
countries: United States
coordinates: lat: 46.7269
lon: -90.785
surface_form: long island
instance_of: Landform
countries: United States
coordinates: lat: 46.7269
lon: -90.785
The tunnels' purpose is to reduce road congestion in the Haifa area and to provide an alternative route for reaching the eastern and central parts of the city, Haifa Bay and the Krayot area to and from Israel's central coastal plain without having to travel through traffic-congested downtown Haifa, having to drive up and across Mount Carmel, or bypassing Haifa from the east – along the edge of the Jezreel Valley (via Highway 70 for example).

Geographic entities mentioned:
surface_form: Jezreel Valley
instance_of: Valley
countries: Israel
coordinates: lat: 32.596388888889
lon: 35.241944444444
Jebel Barkal Museum. The Jebel Barkal Museum is an archaeological site museum located on the eastern side of the archaeological area of Jebel Barkal at Karima in the Northern State of Sudan. Displays.

Geographic entities mentioned:
surface_form: Jebel Barkal
instance_of: Mountain
countries: Sudan
coordinates: lat: 18.5368
lon: 31.8276
Eidsborg. Eidsborg is a village in Tokke Municipality in Telemark county, Norway. The village is located about north of the village of Dalen and the lake Bandak. The village lies in a bowl-shaped valley, surrounded by forests. The 13th-century Eidsborg Stave Church is located in the village. The village is also the site of the Vest-Telemark Museum.

Geographic entities mentioned:
surface_form: Bandak
instance_of: Lake
countries: Norway
coordinates: lat: 59.383333333333
lon: 8.3
Debundscha. Debundscha is a village in the south-western Region of the republic of Cameroon. It is found at the foot of the Mount Cameroon at its south western corner directly facing the south Atlantic Ocean on the Cameroon coast. Debundscha has an extremely wet climate with about of rainfall falling annually.

Geographic entities mentioned:
surface_form: Mount Cameroon
instance_of: Mountain
countries: Cameroon
coordinates: lat: 4.2166666666667
lon: 9.1725
Its height is frequently given as about, but occasionally also as only around. Location. The mountain lies northeast of the Brocken, the highest elevation in the Harz, about 200 m east of the road way from Drei Annen Hohne to Plessenburg. History. Over 100 years ago the Harz Club erected on the summit of the Wolfsklippen one of four iron observation platforms in the Harz that still exist.

Geographic entities mentioned:
surface_form: Brocken
instance_of: Mountain
countries: Germany
Kingdom of Prussia
coordinates: lat: 51.800555555556
lon: 10.617222222222
Wolfsklippen. The Wolfsklippen, also called the Wolfsklippe, is a granite mountain in the Harz mountains in Central Germany with an observation platform on the summit. Its height is frequently given as about, but occasionally also as only around. Location.

Geographic entities mentioned:
surface_form: wolfsklippen
instance_of: Mountain
countries: Germany
coordinates: lat: 51.818888888889
lon: 10.672777777778
Location. The mountain lies northeast of the Brocken, the highest elevation in the Harz, about 200 m east of the road way from Drei Annen Hohne to Plessenburg. History. Over 100 years ago the Harz Club erected on the summit of the Wolfsklippen one of four iron observation platforms in the Harz that still exist. At that time it had a good view of the Brocken and towards Ilsenburg and Wernigerode.

Geographic entities mentioned:
surface_form: wolfsklippen
instance_of: Mountain
countries: Germany
coordinates: lat: 51.818888888889
lon: 10.672777777778
Today this outlook is no longer visible due to the tall spruce trees that block the view. Name and legend. AT the Wolfsklippen the last wolf in the area is supposed to have been killed, which is where the name of the mountain comes from. According to another legend, the name of the crags comes from the witch hunting period, when a girl accused of witchcraft hid here with a she-wolf. Walking.

Geographic entities mentioned:
surface_form: wolfsklippen
instance_of: Mountain
countries: Germany
coordinates: lat: 51.818888888889
lon: 10.672777777778
AT the Wolfsklippen the last wolf in the area is supposed to have been killed, which is where the name of the mountain comes from. According to another legend, the name of the crags comes from the witch hunting period, when a girl accused of witchcraft hid here with a she-wolf. Walking. The Wolfsklippen is check point no. 24 on the walking trail network known as the Harzer Wandernadel.

Geographic entities mentioned:
surface_form: wolfsklippen
instance_of: Mountain
countries: Germany
coordinates: lat: 51.818888888889
lon: 10.672777777778
History. Aid climbing traces its origins to the start of all climbing, with ladders used on historic ascents such as the 1492 ascent of Mont Aiguille, the 1786 ascent of Mont Blanc, or the 1893 ascent of Devils Tower, and with drilled bolts on historic ascents such as the 1875 first ascent of Half Dome. By the start of the 20th century, the widespread use of aid (e.g.

Geographic entities mentioned:
surface_form: Mont Aiguille
instance_of: Mountain
countries: France
coordinates: lat: 44.841944444444
lon: 5.5525
surface_form: Mont Blanc
instance_of: Mountain
countries: France
Italy
coordinates: lat: 45.83277777777778
lon: 6.865
surface_form: Devils Tower
instance_of: Mountain
countries: United States
coordinates: lat: 44.590277777778
lon: -104.71527777778
surface_form: Half Dome
instance_of: Mountain
countries: United States
coordinates: lat: 37.746
lon: -119.53316666667
1970 saw one of the most infamous events in big wall aid climbing with the creation of Cesare Maestri's &quot;Compressor Route&quot; on Cerro Torre. Maestri drilled an extreme amount of bolts into the famous headwall using a 300-pound air compressor drill; in one section, he drilled across a blank 90-metre face to avoid the wind. Maestri's excessive use of aid was condemned.

Geographic entities mentioned:
surface_form: Cerro Torre
instance_of: Mountain
countries: Chile
Argentina
coordinates: lat: -49.2906
lon: -73.09901
MacKay Peak. MacKay Peak is an ice-covered pyramidal peak rising to 770 m in Friesland Ridge, Tangra Mountains, Livingston Island in the South Shetland Islands, Antarctica. It is linked by Pleven Saddle to Tervel Peak to the east-northeast, and surmounts Peshtera Glacier to the north and Charity Glacier to the south.

Geographic entities mentioned:
surface_form: Tervel Peak
instance_of: Mountain
coordinates: lat: -62.717138888889
lon: -60.269444444444
surface_form: charity
instance_of: Mountain
coordinates: lat: -69.9
lon: -64.5667
Location. The peak is located at which is 5.67 km south of Napier Peak, 3.62 km southwest of Kikish Crag, 2.76 km west-southwest of St. Methodius Peak and 2.41 km north-northeast of Veleka Peak (British mapping in 1968, and Bulgarian mapping in 2005 and 2009).

Geographic entities mentioned:
surface_form: Napier Peak
instance_of: Mountain
coordinates: lat: -62.6715
lon: -60.3251
surface_form: Kikish Crag
instance_of: Mountain
coordinates: lat: -62.695
lon: -60.25694444
surface_form: St. Methodius Peak
instance_of: Mountain
coordinates: lat: -62.715833333333
lon: -60.246388888889
surface_form: kikish crag
instance_of: Mountain
coordinates: lat: -62.695
lon: -60.25694444
surface_form: napier peak
instance_of: Mountain
coordinates: lat: -62.6715
lon: -60.3251
surface_form: st. methodius peak
instance_of: Mountain
coordinates: lat: -62.715833333333
lon: -60.246388888889
The peak is named after Captain Donald MacKay, Master of the American shallop &quot;Sarah&quot; who, while seal hunting in the islands in 1820–21, sent home a collection of minerals and rocks to the New York Lyceum of Natural History, forerunner of the American Museum of Natural History. Location.

Geographic entities mentioned:
surface_form: donald
instance_of: Mountain
coordinates: lat: -65.0833
lon: -60.1
MacKay Peak. MacKay Peak is an ice-covered pyramidal peak rising to 770 m in Friesland Ridge, Tangra Mountains, Livingston Island in the South Shetland Islands, Antarctica. It is linked by Pleven Saddle to Tervel Peak to the east-northeast, and surmounts Peshtera Glacier to the north and Charity Glacier to the south.

Geographic entities mentioned:
surface_form: mackay peak
instance_of: Mountain
coordinates: lat: -62.7211
lon: -60.2993
The surrounding neighborhood is urban and densely developed, primarily with attached residential two-story houses built in the late 19th century in the architectural styles of that era, on streets lined with shade trees. Reflecting the proximity of Lake Michigan, the neighborhood is flat. The building itself is similar to its attached neighbors.

Geographic entities mentioned:
surface_form: Lake Michigan
instance_of: Lake
countries: United States
coordinates: lat: 44.007874
lon: -86.756451
North Yuba River. The North Yuba River (also called the North Fork Yuba River) is the main tributary of the Yuba River in northern California in the United States. The river is about long and drains from the Sierra Nevada westwards towards the foothills between the mountains and the Sacramento Valley. It rises on the Sierra Crest about northwest of Sierraville.

Geographic entities mentioned:
surface_form: Sacramento Valley
instance_of: Valley
countries: United States
coordinates: lat: 39
lon: -121.5
Forge Valley railway station. Forge Valley railway station was situated on the North Eastern Railway's Pickering to Seamer branch line. It served the twin villages of East and West Ayton, and the local beauty spot Forge Valley. History. The station opened to passenger traffic on 1 May 1882.

Geographic entities mentioned:
surface_form: Forge Valley
instance_of: Valley
countries: United Kingdom
coordinates: lat: 54.2699
lon: -0.489654
Menosgada. Menosgada (&quot;town above the Main valley&quot;) was a Celtic metropolis on the Upper Main (river) that was mentioned by the Greek geographer, Ptolemy. It was probably located on the hill known today as the Staffelberg. In the 1st millennium BC, Celts settled on the Staffelberg.

Geographic entities mentioned:
surface_form: Staffelberg
instance_of: Mountain
countries: Germany
coordinates: lat: 50.092222222222
lon: 11.024722222222
In the centre of the site is an acropolis measuring 3 hectares in area. Menosgada met its demise around 50 BC when the Romans tried unsuccessfully to advance eastwards along the Main graben to the Elbe river, but ran into massive opposition from the Germanic tribes. The times were too turbulent, and the site was abandoned by its inhabitants.

Geographic entities mentioned:
surface_form: Elbe
instance_of: Watercourse
countries: Czech Republic
Germany
coordinates: lat: 53.922222222222224
lon: 8.722222222222221
Sailing at the 2022 Bolivarian Games. Sailing competitions at the 2022 Bolivarian Games in Valledupar, Colombia were held from 27 June to 2 July 2022 at Tominé Reservoir in Guatavita, a sub-venue outside Valledupar. Seven medal events were scheduled to be contested; three for men, three for women and one mixed event. A total of 73 athletes (36 men and 37 women) will compete in the events.

Geographic entities mentioned:
surface_form: Tominé Reservoir
instance_of: Lake
countries: Colombia
coordinates: lat: 4.954
lon: -73.84
Each nation could register up to two sailors for each men and women singles events and up to two teams conformed by one man and two women each for the mixed event. Venue. The sailing competitions were held at the Tominé Reservoir at kilometer 10 on the Sesquile - Gutavita road in Guatavita, a municipality of Cundinamarca Department.

Geographic entities mentioned:
surface_form: Tominé Reservoir
instance_of: Lake
countries: Colombia
coordinates: lat: 4.954
lon: -73.84
The Oxnard Plain faces the Santa Barbara Channel portion of the Southern California Bight, extending from the abrupt transition of the steep rocky shore at Point Mugu in the Santa Monica Mountains on the south to the Ventura River on the north. Prominent on the southeastern horizon are Conejo Mountain and Boney Peak.

Geographic entities mentioned:
surface_form: Conejo Mountain
instance_of: Mountain
countries: United States
coordinates: lat: 34.18833333
lon: -118.98444444
surface_form: Boney Peak
instance_of: Mountain
countries: United States
coordinates: lat: 34.1163
lon: -118.94
After years of legal tussles, the McGrath Peaker Plant was built by Edison next to the power plant at Mandalay. Geography. This plain is bounded by the Santa Monica Mountains, the Santa Susana Mountains, the Topatopa Mountains to the north, the Santa Clara River Valley to the northeast and the Santa Barbara Channel to the south and west. The topography of the plain is relatively level.

Geographic entities mentioned:
surface_form: Santa Clara River Valley
instance_of: Valley
countries: United States
coordinates: lat: 34.3667
lon: -118.983
The topography of the plain is relatively level. It has been formed chiefly by the deposition of sediments from Santa Clara River Valley and the watershed of Calleguas Creek before they flow into the Pacific Ocean. The alluvial deposits from these rivers are generally a few hundred feet () thick and lie over Pleistocene and Pliocene sedimentary rocks.

Geographic entities mentioned:
surface_form: Santa Clara River Valley
instance_of: Valley
countries: United States
coordinates: lat: 34.3667
lon: -118.983
The city held a ribbon cutting ceremony in November 2021 as the plant began to operate. After extensive testing and adjustments, the plant started producing water for the city in January 2023. The Camrosa Water District serves nearly 30,000 people in Camarillo and the Santa Rosa Valley along with agricultural customers. The district, which covers is headquartered in Camarillo.

Geographic entities mentioned:
surface_form: Santa Rosa Valley
instance_of: Valley
countries: United States
coordinates: lat: 34.2439
lon: -118.897
Oxnard Plain. The Oxnard Plain is a large coastal plain in southwest Ventura County, California, United States surrounded by the mountains of the Transverse Ranges. The cities of Oxnard, Camarillo, Port Hueneme and much of Ventura as well as the unincorporated communities of Hollywood Beach, El Rio, Saticoy, Silver Strand Beach, and Somis lie within the over.

Geographic entities mentioned:
surface_form: silver strand
instance_of: Landform
countries: United States
coordinates: lat: 32.6466
lon: -117.148
Oxnard Plain. The Oxnard Plain is a large coastal plain in southwest Ventura County, California, United States surrounded by the mountains of the Transverse Ranges. The cities of Oxnard, Camarillo, Port Hueneme and much of Ventura as well as the unincorporated communities of Hollywood Beach, El Rio, Saticoy, Silver Strand Beach, and Somis lie within the over.

Geographic entities mentioned:
surface_form: oxnard plain
instance_of: Valley
countries: United States
coordinates: lat: 34.36
lon: -119.15
The is among the longest stretches of continuous, linear beaches in the state. The high quality soils, adequate water supply, favorable climate, long growing season, and level topography are characteristic of the Oxnard Plain where the top cash crops are strawberries, raspberries, nursery stock and celery.

Geographic entities mentioned:
surface_form: oxnard plain
instance_of: Valley
countries: United States
coordinates: lat: 34.36
lon: -119.15
The Oxnard Plain faces the Santa Barbara Channel portion of the Southern California Bight, extending from the abrupt transition of the steep rocky shore at Point Mugu in the Santa Monica Mountains on the south to the Ventura River on the north. Prominent on the southeastern horizon are Conejo Mountain and Boney Peak.

Geographic entities mentioned:
surface_form: oxnard plain
instance_of: Valley
countries: United States
coordinates: lat: 34.36
lon: -119.15
Prominent on the southeastern horizon are Conejo Mountain and Boney Peak. The Oxnard Plain contains a considerable petroleum reserve with several active oil fields – the Oxnard Oil Field, east of Oxnard, the West Montalvo Oil Field, along the coast south of the outlet of the Santa Clara River, and the Santa Clara Avenue Oil Field north of U.S. Highway 101 near El Rio.

Geographic entities mentioned:
surface_form: oxnard plain
instance_of: Valley
countries: United States
coordinates: lat: 34.36
lon: -119.15
Mission San Buenaventura was founded in 1782 next to the Ventura River, upcoast from the Santa Clara River. The Oxnard plain was used for grazing herds of livestock which required thousands of acres. The traditional way of life of the Chumash people became increasingly unstable and unsustainable on the Oxnard Plain with the introduction of these animals.

Geographic entities mentioned:
surface_form: oxnard plain
instance_of: Valley
countries: United States
coordinates: lat: 34.36
lon: -119.15
Most of the arable land was divided up into large ranchos by 1846. This opened up the Oxnard Plain to further settlement by Europeans. Control of the area was transferred to the United States under the Treaty of Guadalupe Hidalgo in 1848 and California became the 31st state in the Union in 1850. Many Mexican residents and residents who had immigrated from European countries became U.S. citizens.

Geographic entities mentioned:
surface_form: oxnard plain
instance_of: Valley
countries: United States
coordinates: lat: 34.36
lon: -119.15
In 1911, J. Smeaton Chase noted the &quot;prosperous fields of beans and beets&quot; as he descended from the Santa Monica Mountains onto the Oxnard Plain during his horseback journey from Mexico to Oregon.

Geographic entities mentioned:
surface_form: oxnard plain
instance_of: Valley
countries: United States
coordinates: lat: 34.36
lon: -119.15
The once busy port had drastically declined as passenger and freight traffic shifted to the railroad. Postwar and modern development. Although agriculture has long been important to the economy on the Oxnard Plain, the booming growth in the 1960s of the cities located on the plain expanding by building housing, highways, and associated infrastructure over the rich agricultural land.

Geographic entities mentioned:
surface_form: oxnard plain
instance_of: Valley
countries: United States
coordinates: lat: 34.36
lon: -119.15
They continued to use the sites until they were closed in 1996. Municipal wastewater treatment facilities, industrial dischargers, and power generating stations are point source dischargers along the coast of the Oxnard plain. Water quality at the numerous beaches has been very good with a few exceptions.

Geographic entities mentioned:
surface_form: oxnard plain
instance_of: Valley
countries: United States
coordinates: lat: 34.36
lon: -119.15
Prior to the agricultural expansion, installation of drainage systems, and other disturbances, this broad, flat, coastal area contained a series of marshes, salt flats, sloughs, and lagoons. Historically, Calleguas Creek flood flows spread across the floodplain and the deposited sediment created the rich agricultural lands of the Oxnard Plain.

Geographic entities mentioned:
surface_form: oxnard plain
instance_of: Valley
countries: United States
coordinates: lat: 34.36
lon: -119.15
Groundwater. Saltwater intrusion from the ocean has occurred in the southern Oxnard Plain due to the overdraft of groundwater. The Santa Clara Irrigating Company was formed in 1870 and drew water from the Santa Clara River, using a ditch system to irrigate the grain crops. Early settlers began pumping soon afterwards to support farming activities with what at first was a more reliable source.

Geographic entities mentioned:
surface_form: oxnard plain
instance_of: Valley
countries: United States
coordinates: lat: 34.36
lon: -119.15
The Sustainable Groundwater Management Act signed into California law in 2014 created a framework for sustainable, local groundwater management for the first time in California history. In response, the Ventura County Board of Supervisors passed an emergency ordinance that halted well-drilling in the Oxnard Plain. Groundwater levels experienced a decrease during the 2012–2013 drought.

Geographic entities mentioned:
surface_form: oxnard plain
instance_of: Valley
countries: United States
coordinates: lat: 34.36
lon: -119.15
Calleguas Municipal Water District. Calleguas Municipal Water District, a water wholesaler, serves about 75 percent of Ventura County's population. Calleguas ships state water from the Delta to Oxnard, Port Hueneme, and Camarillo on the Oxnard Plain and Moorpark, Thousand Oaks, Simi Valley and unincorporated areas in the east county.

Geographic entities mentioned:
surface_form: oxnard plain
instance_of: Valley
countries: United States
coordinates: lat: 34.36
lon: -119.15
The source of the salts is a combination of agricultural, industrial, and residential activities in conjunction with salts in the imported water. The United Water Conservation District funded a detailed feasibility study in 2014 and found that the impaired groundwater in the south Oxnard Plain is suitable for treatment by reverse osmosis at an acceptable recovery range of 72 to 80 percent.

Geographic entities mentioned:
surface_form: oxnard plain
instance_of: Valley
countries: United States
coordinates: lat: 34.36
lon: -119.15
The District encompasses about and owns Lake Piru and key facilities along the Santa Clara River that are used to manage groundwater supplies. The United Water Conservation District provides wholesale water delivery through three pipelines to various portions of the Oxnard Plain.

Geographic entities mentioned:
surface_form: oxnard plain
instance_of: Valley
countries: United States
coordinates: lat: 34.36
lon: -119.15
One is the Oxnard/Hueneme system which serves the City of Oxnard, the Port Hueneme Water Agency (City of Port Hueneme, Channel Islands Beach CSD) and the Naval Base Ventura County (Point Mugu and the Construction Battalion Center). A second pipeline serves agricultural uses in the Oxnard Plain. The third system supplies water to the Pleasant Valley area located between Oxnard and Camarillo.

Geographic entities mentioned:
surface_form: oxnard plain
instance_of: Valley
countries: United States
coordinates: lat: 34.36
lon: -119.15
The National Marine Fisheries Service determined that fixing this was a high priority since it is the first structure the steelhead encounter when attempting to migrate from the ocean. United released water from Lake Piru to specifically recharge the Fox Canyon in the Oxnard Plain for the first time in 2019. Ormond Beach.

Geographic entities mentioned:
surface_form: oxnard plain
instance_of: Valley
countries: United States
coordinates: lat: 34.36
lon: -119.15
United released water from Lake Piru to specifically recharge the Fox Canyon in the Oxnard Plain for the first time in 2019. Ormond Beach. Ormond Beach is a broad, flat, coastal area on the south side of the Oxnard Plain that historically contained marshes, salt flats, sloughs, and lagoons.

Geographic entities mentioned:
surface_form: oxnard plain
instance_of: Valley
countries: United States
coordinates: lat: 34.36
lon: -119.15
Forge Valley. Forge Valley is a national nature reserve in North Yorkshire, England, located within the North York Moors National Park on the East Ayton / Hackness road. The valley follows the route of the River Derwent and was formed by melting ice water at the end of the last ice age. The NNR at Forge Valley covers over.

Geographic entities mentioned:
surface_form: forge valley
instance_of: Valley
countries: United Kingdom
coordinates: lat: 54.2699
lon: -0.489654
Forge Valley is a national nature reserve in North Yorkshire, England, located within the North York Moors National Park on the East Ayton / Hackness road. The valley follows the route of the River Derwent and was formed by melting ice water at the end of the last ice age. The NNR at Forge Valley covers over. The area is now covered with woodlands which are thought to be 6,000 years old.

Geographic entities mentioned:
surface_form: forge valley
instance_of: Valley
countries: United Kingdom
coordinates: lat: 54.2699
lon: -0.489654
The NNR at Forge Valley covers over. The area is now covered with woodlands which are thought to be 6,000 years old. Forge Valley takes its name from the fact that charcoal was produced in these woods, for use in iron forges. There was a foundry to the north of the valley in 1798. Forge Valley is managed by Raincliffe Woods Community Enterprise CIC.

Geographic entities mentioned:
surface_form: forge valley
instance_of: Valley
countries: United Kingdom
coordinates: lat: 54.2699
lon: -0.489654
Caliente Range. The Caliente Range is a west-east trending zone of uplift mountains in the California Coast Ranges, in central California. The highest peak of the range is Caliente Mountain at in elevation, located in southeastern San Luis Obispo County. Geology.

Geographic entities mentioned:
surface_form: Caliente Mountain
instance_of: Mountain
countries: United States
coordinates: lat: 35.0364
lon: -119.76
Geology. The range is an anticlinal structure with a sharp southern boundary defined by the Morales Thrust Fault, along which runs the Cuyama River. The Cuyama Valley separates the Caliente Range from the Sierra Madre Mountains in neighboring Santa Barbara County to the south. To the northeast, the range is bounded by the Carrizo Plain.

Geographic entities mentioned:
surface_form: Cuyama Valley
instance_of: Valley
countries: United States
coordinates: lat: 34.9295
lon: -119.597
Emilia Prieto Tugores. Emilia Prieto Tugores (11 January 1902 – 1986) was a graphic artist, educator, singer, composer, and scholar of folklore from the Central Valley of Costa Rica, one of the few women to enter the field of artistic satire in the first half of the 20th century. Her work was recognized with a Joaquín Monge Prize for cultural periodism in the 1984.

Geographic entities mentioned:
surface_form: Central Valley of Costa Rica
instance_of: Valley
countries: Costa Rica
coordinates: lat: 9.91667
lon: -84.0667
There is another Anglican church at Llanrothal. The area contains a lot of history, including Pembridge Castle and at least thirty-one other archaeological sites in Welsh Newton parish alone. The parish also contains a piece of common land, currently registered as unowned under the Commons Act 2006, at Welsh Newton Common; a hill (and hamlet) overlooking the Wye Valley.

Geographic entities mentioned:
surface_form: Wye Valley
instance_of: Valley
countries: United Kingdom
coordinates: lat: 51.69255
lon: -2.66283
Waun Fach is, with a summit height of, the highest mountain in the Black Mountains in south-eastern Wales. It is one of the three Marilyns over 600 m that make up the range, the others being Black Mountain and Mynydd Troed. To the north Rhos Fawr and the Radnor Forest can be seen. It is the third highest mountain in Britain south of Snowdonia (after Pen y Fan and its near neighbour Corn Du).

Geographic entities mentioned:
surface_form: Rhos Fawr
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 52.2671
lon: -3.1998
It is one of the three Marilyns over 600 m that make up the range, the others being Black Mountain and Mynydd Troed. To the north Rhos Fawr and the Radnor Forest can be seen. It is the third highest mountain in Britain south of Snowdonia (after Pen y Fan and its near neighbour Corn Du). It is situated at the head of the Grwyne Fechan valley, above and to the west of the Grwyne Fawr reservoir.

Geographic entities mentioned:
surface_form: Pen y Fan
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 51.884031
lon: -3.436765
It is situated at the head of the Grwyne Fechan valley, above and to the west of the Grwyne Fawr reservoir. It has an undistinguished (and almost indistinguishable) rounded summit. The nearby tops on the ridge, Pen Trumau and Pen y Gadair Fawr, although lower, are very much more recognisable. Geology.

Geographic entities mentioned:
surface_form: Pen y Gadair Fawr
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 51.951961
lon: -3.12264
surface_form: pen y gadair
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 52.699827777778
lon: -3.9086944444444
Waun Fach. Waun Fach is, with a summit height of, the highest mountain in the Black Mountains in south-eastern Wales. It is one of the three Marilyns over 600 m that make up the range, the others being Black Mountain and Mynydd Troed. To the north Rhos Fawr and the Radnor Forest can be seen.

Geographic entities mentioned:
surface_form: black mountain
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 51.8814
lon: -3.70848
surface_form: black mountain
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.6
lon: -5.98
surface_form: black mountain
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 52.008333333333
lon: -3.0847222222222
Waun Fach. Waun Fach is, with a summit height of, the highest mountain in the Black Mountains in south-eastern Wales. It is one of the three Marilyns over 600 m that make up the range, the others being Black Mountain and Mynydd Troed. To the north Rhos Fawr and the Radnor Forest can be seen.

Geographic entities mentioned:
surface_form: waun fach
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 51.96279
lon: -3.14319
The nearby tops on the ridge, Pen Trumau and Pen y Gadair Fawr, although lower, are very much more recognisable. Geology. The summit and upper slopes of Waun Fach are formed from the Early Devonian Epoch sandstones of the Brownstones Formation, a division of the Old Red Sandstone. Beneath these and forming the lower slopes are the sandstones of the Senni Formation (traditionally the Senni Beds).

Geographic entities mentioned:
surface_form: waun fach
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 51.96279
lon: -3.14319
This configuration makes them excellent at capturing and storing water. Hence they serve an important role as aquifers across much of Northern Europe, Canada and the United States. Examples include Oak Ridges Moraine Aquifer, Spokane Valley-Rathdrum Prairie Aquifer, Mahomet Aquifer, the Saginaw Lobe Aquifer, and the Corning Aquifer. Buried, open and partially filled.

Geographic entities mentioned:
surface_form: Oak Ridges Moraine Aquifer
instance_of: Mountain
countries: Canada
coordinates: lat: 44.05
lon: -78.86666667
They can exhibit reverse gradients, which result when pressurized meltwater flows over obstacles such as ridges or hills along the glacier bed. Tunnel valleys can be formed under extremely thick glacial ice – examples have been observed on the bottom of Lake Superior and in the oceans offshore in Antarctica.

Geographic entities mentioned:
surface_form: Lake Superior
instance_of: Lake
countries: Canada
United States
coordinates: lat: 47.52881611111111
lon: -87.76002194444445
They are found extensively in the United Kingdom with several examples reported from Cheshire for example. They are also to be found under the North Sea. Examples of lakes formed in tunnel valleys include the Ruppiner See (a lake in Ostprignitz-Ruppin, Brandenburg), the Werbellinsee, and the Schwielochsee, all in Germany. North America.

Geographic entities mentioned:
surface_form: Ruppiner See
instance_of: Lake
countries: Germany
coordinates: lat: 52.8975
lon: 12.8075
North America. Okanagan Lake is a large, deep ribbon lake in the Okanagan Valley of British Columbia which formed in a tunnel valley from the Okanogan lobe of the Cordilleran Ice Sheet. The lake is long, between wide, and has a surface area of. Northern Idaho and Montana show evidence of tunnel valley formation under the Purcell lobe and the Flathead Lobe of the Cordilleran Ice Sheet.

Geographic entities mentioned:
surface_form: Okanagan Lake
instance_of: Lake
countries: Canada
coordinates: lat: 49.920833333333
lon: -119.5
Paul. The Kawartha lakes of Ontario formed in the Late Wisconsinan glacial period. Ice melt from the Niagara Escarpment flowed through tunnel valleys beneath the ice expanded to form a west-to-east passage between the main Laurentide Ice Sheet and a mass of ice in the Lake Ontario basin. Cedar Creek Canyon is a tunnel valley located in Allen County, Indiana.

Geographic entities mentioned:
surface_form: Niagara Escarpment
instance_of: Mountain
countries: Canada
coordinates: lat: 43.8334
lon: -79.99966
surface_form: Lake Ontario
instance_of: Lake
countries: Canada
United States
coordinates: lat: 43.72888888888889
lon: -78.10638888888889
Lawrence River, which is also of glacial origin. Seismic reflection profiles of the fill of tunnel valleys suggest that they are of various ages, with the youngest dating from shortly after the Late Glacial Maximum. They result from erosion by sub-glacial water crossing the eastern Scotian Shelf off Nova Scotia. They originate from the Laurentian Channel south of the Cabot Strait.

Geographic entities mentioned:
surface_form: Cabot Strait
instance_of: Watercourse
countries: Canada
coordinates: lat: 47.233333333333
lon: -59.716666666667
The club was based in Sowerby Bridge, a small market town (population approx. 10,000) that lies within the Upper Calder Valley in the district of Calderdale in West Yorkshire, northern England, and approximately 3 miles from Halifax. The club joined the Northern Union in 1901-02 and played for the single season in the Yorkshire Senior Competition. History.

Geographic entities mentioned:
surface_form: Upper Calder Valley
instance_of: Valley
countries: United Kingdom
coordinates: lat: 53.72
lon: -2.004
Mascoma Lake. Mascoma Lake is a lake in western New Hampshire, United States. Most of the lake is within the town of Enfield, while a small portion is within the city of Lebanon, where it drains into the Mascoma River, a tributary of the Connecticut River. The lake's general trend is from southeast to northwest, with the outlet at the northwestern end.

Geographic entities mentioned:
surface_form: mascoma lake
instance_of: Lake
countries: United States
coordinates: lat: 43.622222222222
lon: -72.140833333333
The lake freezes during winter and is stable enough to be walked upon. Ice fishing is popular on the lake. The lake is stocked with trout by the New Hampshire Fish and Game Department. Mascoma Lake often has a spring cyanobacteria bloom. Recent studies suggest that significant exposure to high levels of cyanobacteria producing toxins such as BMAA can cause amyotrophic lateral sclerosis (ALS).

Geographic entities mentioned:
surface_form: mascoma lake
instance_of: Lake
countries: United States
coordinates: lat: 43.622222222222
lon: -72.140833333333
Aside from the bloom, the lake is generally considered safe for swimming, and the town of Enfield maintains a public beach with a lifeguard on the lake. NASA and its partners have used the frozen lake to test a robotic rover as a simulation of Antarctica. Mascoma Lake is home to the Dartmouth College sailing team. A community sailing club called the Mascoma Sailing Club also uses the lake.

Geographic entities mentioned:
surface_form: mascoma lake
instance_of: Lake
countries: United States
coordinates: lat: 43.622222222222
lon: -72.140833333333
Piz Chaschauna. Piz Chaschauna (also known as Piz Casana) is a mountain of the Livigno Alps, located on the border between Italy and Switzerland. The northern side of the mountain (Graubünden) is part of the Swiss National Park. The eastern side of the mountain (Lombardy) is part of the Stelvio National Park.

Geographic entities mentioned:
surface_form: piz chaschauna
instance_of: Mountain
countries: Switzerland
Italy
coordinates: lat: 46.575277777778
lon: 10.078611111111
Piz Chaschauna. Piz Chaschauna (also known as Piz Casana) is a mountain of the Livigno Alps, located on the border between Italy and Switzerland. The northern side of the mountain (Graubünden) is part of the Swiss National Park. The eastern side of the mountain (Lombardy) is part of the Stelvio National Park.

Geographic entities mentioned:
surface_form: piz chaschauna
instance_of: Mountain
countries: Switzerland
Italy
coordinates: lat: 46.575277777778
lon: 10.078611111111
surface_form: piz casana
instance_of: Mountain
countries: Switzerland
Italy
coordinates: lat: 46.575277777778
lon: 10.078611111111
Its natural habitats are wet lowland forests of Sri Lanka. This frog is active at night, but people have seen it during the day in shaded perches on rocks. It is threatened by habitat loss, which scientists attribute to urbanization, increased agriculture and grazing, and logging. It is one of the 8 species of rhacophorids that was discovered from Adam's Peak in 2013. Etymology.

Geographic entities mentioned:
surface_form: Adam's Peak
instance_of: Mountain
countries: Sri Lanka
coordinates: lat: 6.809444444444445
lon: 80.49972222222222
It is larger than either of the states of Rhode Island (1544.9 square miles) or the state of Delaware (2488.72 square miles). St. Lawrence County is part of the North Country region. Part of the county is in the Adirondack Park. It includes much of the Oswegatchie River, Cranberry Lake and Lake Ozonia. The Port of Ogdensburg in St. Lawrence County is the only U.S. port on the St. Lawrence Seaway.

Geographic entities mentioned:
surface_form: Cranberry Lake
instance_of: Lake
countries: United States
coordinates: lat: 44.172222222222
lon: -74.823888888889
surface_form: Lake Ozonia
instance_of: Lake
countries: United States
coordinates: lat: 44.5992
lon: -74.6164
&quot;Tephrosia purpurea&quot; is also found in the United Arab Emirates and in Oman, where it inhabits the Jiddat al-Harasis desert and dominates the beds of wadis in mountains such as Jebel Shams. Toxicity.

Geographic entities mentioned:
surface_form: Jebel Shams
instance_of: Mountain
countries: Oman
coordinates: lat: 23.2373882
lon: 57.2637937
Ashley Creek (Current River tributary). Ashley Creek is a stream in Dent and Texas counties in the Ozarks of southern Missouri. It is a tributary to the Current River. The creek is formed by the joining of North Ashley Creek and South Ashley Creek. The junction of the two tributaries is at and the confluence with the Current River is at.

Geographic entities mentioned:
surface_form: Ozarks
instance_of: Plateau
countries: United States
coordinates: lat: 37.1822
lon: -92.5159
surface_form: ashley creek
instance_of: Watercourse
countries: United States
coordinates: lat: 37.42805556
lon: -91.64972222
surface_form: the ozarks
instance_of: Plateau
countries: United States
coordinates: lat: 37.1822
lon: -92.5159
Ashley Creek (Current River tributary). Ashley Creek is a stream in Dent and Texas counties in the Ozarks of southern Missouri. It is a tributary to the Current River. The creek is formed by the joining of North Ashley Creek and South Ashley Creek. The junction of the two tributaries is at and the confluence with the Current River is at.

Geographic entities mentioned:
surface_form: ashley creek (current river tributary)
instance_of: Watercourse
countries: United States
coordinates: lat: 37.42805556
lon: -91.64972222
Ashley Creek is a stream in Dent and Texas counties in the Ozarks of southern Missouri. It is a tributary to the Current River. The creek is formed by the joining of North Ashley Creek and South Ashley Creek. The junction of the two tributaries is at and the confluence with the Current River is at. The stream system has the name of William Henry Ashley, a frontiersman.

Geographic entities mentioned:
surface_form: ashley creek
instance_of: Watercourse
countries: United States
coordinates: lat: 37.42805556
lon: -91.64972222
surface_form: ashley creek
instance_of: Watercourse
countries: United States
coordinates: lat: 37.42805556
lon: -91.64972222
Distribution and habitat. The Ibiza wall lizard is native to the islands of Ibiza and Formentera in the Balearic Islands and the neighbouring rocky islets. It has been introduced to Muella de Palma (Mallorca), Barcelona where it once was assumed it died out but was 're-discovered' in 2007 (Bruekers, 2007) in the town of Aleria in southern Spain and the island of Gaztelugatxe in northern Spain.

Geographic entities mentioned:
surface_form: Gaztelugatxe
instance_of: Mountain
countries: Spain
coordinates: lat: 43.447
lon: -2.785
Lake Wolayer. The Lake Wolayer is an Austrian mountain lake on the Carinthian side of the, near the Plöcken Pass. It is the centrepiece of the Wolayer See and surrounding area nature reserve. Notable plant species include Alpine eryngo (&quot;Eryngium alpestre&quot;), sweet cicely (&quot;Myrrhis odorata&quot;), and Austrian ribwort (&quot;Pleurospermum austriacum&quot;).

Geographic entities mentioned:
surface_form: lake wolayer
instance_of: Lake
countries: Austria
coordinates: lat: 46.61111111
lon: 12.86916667
Lake Wolayer. The Lake Wolayer is an Austrian mountain lake on the Carinthian side of the, near the Plöcken Pass. It is the centrepiece of the Wolayer See and surrounding area nature reserve. Notable plant species include Alpine eryngo (&quot;Eryngium alpestre&quot;), sweet cicely (&quot;Myrrhis odorata&quot;), and Austrian ribwort (&quot;Pleurospermum austriacum&quot;).

Geographic entities mentioned:
surface_form: wolayer see
instance_of: Lake
countries: Austria
coordinates: lat: 46.61111111
lon: 12.86916667
Biology. Due to the low nutrient concentration, the amount of suspended algae is minimal, measuring less than 250 mg/m3. Like most high mountain lakes, Wolayer See is naturally fish-free. However, in 1976, 15 brown trout were introduced, significantly reducing the population of lake fleas (&quot;Gammarus lacustris&quot;).

Geographic entities mentioned:
surface_form: wolayer see
instance_of: Lake
countries: Austria
coordinates: lat: 46.61111111
lon: 12.86916667
Haughom Chapel. Haughom Church () is a parish church of the Church of Norway in the large Sirdal Municipality in Agder county, Norway. It is located in the village of Haughom on the eastern shore of the lake Sirdalsvatnet. It one of the four churches in the Sirdal parish which is part of the Lister og Mandal prosti (deanery) in the Diocese of Agder og Telemark.

Geographic entities mentioned:
surface_form: Sirdalsvatnet
instance_of: Lake
countries: Norway
coordinates: lat: 58.4675
lon: 6.67638889
Geography. According to the U.S. Census Bureau, the county has a total area of, of which is land and (5.7%) is water. The county is divided between the Ozark Plateau in the north and the Ouachita Mountains in the south. The Cookson Hills are in the northwest part of the county. The Arkansas River forms the southern border. Other major waterways are the Illinois River and Robert S. Kerr Reservoir.

Geographic entities mentioned:
surface_form: Cookson Hills
instance_of: Landform
countries: United States
coordinates: lat: 35.7
lon: -94.8
It flows northward into Lake Turkana. It is one of the longest rivers in Kenya (about), originating near the equator. Course. The Kerio River rises on the north slopes of the Amasya Hills to the west of Lake Bogoria. It flows northward through the Kerio Valley between Tugen Hills and Elgeyo Escarpment. The Elgeyo Escarpment rises to over above the Kerio valley in places.

Geographic entities mentioned:
surface_form: Kerio Valley
instance_of: Valley
countries: Kenya
coordinates: lat: 0.6401
lon: 35.6086
It is drained to the south by Summers Glacier and to the west by Montecchi Glacier. Features include Boss Peak and Bridwell Peak in the north, Mount Hazlett and Latino Peak in the southeast. Boss Peak. An isolated black peak high at the east side of the terminus of Jutland Glacier, north-northeast of Thomson Peak, in the northwest part of the Victory Mountains.

Geographic entities mentioned:
surface_form: Thomson Peak
instance_of: Mountain
coordinates: lat: -71.9833
lon: 166.117
Crotch Hill. Crotch Hill is a summit in Hancock County, Maine, in the United States. With an elevation of, Crotch Hill is the 1656th tallest mountain in Maine.

Geographic entities mentioned:
surface_form: crotch hill
instance_of: Mountain
countries: United States
coordinates: lat: 44.783878
lon: -68.271963
state of Missouri. It is a tributary of Little Blue River. The stream headwaters arise in northern Cass County at approximately 1.5 miles north of Raymore and flows north-northwest into Jackson County. The stream enters the Little Blue in east Grandview within the upper reaches of Longview Lake at. Lumpkins Fork has the name of the local Lumpkin family.

Geographic entities mentioned:
surface_form: Longview Lake
instance_of: Lake
countries: United States
coordinates: lat: 38.9097
lon: -94.4696
Landslides. The Tauredunum event was a large tsunami on Lake Geneva in 563 CE, caused by sedimentary deposits destabilised by a landslide. In the 1950s, it was discovered that tsunamis larger than had previously been believed possible can be caused by giant submarine landslides. These large volumes of rapidly displaced water transfer energy at a faster rate than the water can absorb.

Geographic entities mentioned:
surface_form: Lake Geneva
instance_of: Lake
countries: Switzerland
France
coordinates: lat: 46.45
lon: 6.55
The wave struck three boats—each with two people aboard—anchored in the bay. One boat rode out the wave, but the wave sank the other two, killing both people aboard one of them. Another landslide-tsunami event occurred in 1963 when a massive landslide from Monte Toc entered the reservoir behind the Vajont Dam in Italy. The resulting wave surged over the -high dam by and destroyed several towns.

Geographic entities mentioned:
surface_form: Monte Toc
instance_of: Mountain
countries: Italy
coordinates: lat: 46.233333333333
lon: 12.333333333333
The resulting wave surged over the -high dam by and destroyed several towns. Around 2,000 people died. Scientists named these waves megatsunamis. Some geologists claim that large landslides from volcanic islands, e.g. Cumbre Vieja on La Palma (Cumbre Vieja tsunami hazard) in the Canary Islands, may be able to generate megatsunamis that can cross oceans, but this is disputed by many others.

Geographic entities mentioned:
surface_form: Cumbre Vieja
instance_of: Mountain
countries: Spain
coordinates: lat: 28.566666666667
lon: -17.833333333333