Sarmila/GeoWiki-Features huggingface dataset:
In the east, the March was covered by the river course of the Oder. The few available Brandenburg soldiers were recalled to fortified locations. In this way, as a result of the prevailing circumstances, Brandenburg's defences were formed along the line from Köpenick, via Berlin, Spandau, Oranienburg, Kremmen, Fehrbellin and Havelberg to the River Elbe.

Geographic entities mentioned:
surface_form: Elbe
instance_of: Watercourse
countries: Czech Republic
Germany
coordinates: lat: 53.922222222222224
lon: 8.722222222222221
The total army number available for the upcoming campaign had thus shrunk to between 11,000 and 12,000 men, by 10 May. Wrangel's goal was to cross the Elbe to link up with Swedish forces in Bremen-Verden and the 13,000 strong army of their ally, John Frederick, Duke of Brunswick and Lunenburg, in order to cut the approach route of the Elector and his army into Brandenburg.

Geographic entities mentioned:
surface_form: Elbe
instance_of: Watercourse
countries: Czech Republic
Germany
coordinates: lat: 53.922222222222224
lon: 8.722222222222221
Bukit Kutu. Bukit Kutu or Treacher Hill is a former hill station and now a ghost town in Hulu Selangor District, Selangor, Malaysia. This hill station was established in 1893 and consisted of two bungalows, which served as a lodge for visitors and included a bridle path that connected it with the town of Kuala Kubu.

Geographic entities mentioned:
surface_form: bukit kutu
instance_of: Mountain
countries: Malaysia
coordinates: lat: 3.5428888888888888
lon: 101.72016666666667
The Japanese army later bombed the station during World War II, leaving it a ghost town. Since the abandonment of the hill station, it has become a popular hiking destination and is busiest during weekends. Bukit Kutu has a rich biodiversity with various kinds of flora and fauna which led to its gazettement as a wildlife reserve in 1922. Etymology.

Geographic entities mentioned:
surface_form: bukit kutu
instance_of: Mountain
countries: Malaysia
coordinates: lat: 3.5428888888888888
lon: 101.72016666666667
Etymology. Treacher Hill is named after a former British Resident of Selangor, William Hood Treacher, whereas the alternative Malayan name Bukit Kutu comes from the &quot;Orang Asli&quot; people who said the route was too long. &quot;Kutu&quot; in Malay language means flea, and &quot;Bukit&quot; means hill, literally &quot;flea hill&quot;. History.

Geographic entities mentioned:
surface_form: bukit kutu
instance_of: Mountain
countries: Malaysia
coordinates: lat: 3.5428888888888888
lon: 101.72016666666667
Occupying them required a permit from the Kuala Kubu District Officer. Each bungalow provided bedrooms, a landline telephone, a fireplace, a tennis court and a telescope. The hill station was connected by a bridle path, which served as the only road connecting Kuala Kubu with Bukit Kutu.

Geographic entities mentioned:
surface_form: bukit kutu
instance_of: Mountain
countries: Malaysia
coordinates: lat: 3.5428888888888888
lon: 101.72016666666667
While police has been attempted to search for the missing person, as of 2019, her remains has yet to be found. One hiker was rescued after they collapsed from a muscle cramp in November 2016. In July 2017, a hiker from Egypt was reportedly missing on Bukit Kutu, only to be rediscovered after 16 hours. Geography. Bukit Kutu is a mountainous terrain.

Geographic entities mentioned:
surface_form: bukit kutu
instance_of: Mountain
countries: Malaysia
coordinates: lat: 3.5428888888888888
lon: 101.72016666666667
The other three are Hulu Selangor, Semangkok and Fraser's Hill. Aside from forests which cover the water catchment areas, the other natural features in Bukit Kutu include the Lata Medang waterfall, and a large stone called Batu Tebung, which was reportedly defaced by irresponsible people who visited the site.

Geographic entities mentioned:
surface_form: bukit kutu
instance_of: Mountain
countries: Malaysia
coordinates: lat: 3.5428888888888888
lon: 101.72016666666667
It takes its name from the village Murdeira, which lies at its shore. At its northwestern end lie the steep cliff of Rabo de Junco and the islet Ilhéu Rabo de Junco. The bay is protected as a marine nature reserve, which covers 182 hectares of land and 5,925 hectares of sea, including the Ilhéu Rabo de Junco. It is a nesting area for sea turtles and seabirds.

Geographic entities mentioned:
surface_form: Rabo de Junco
instance_of: Mountain
countries: Cape Verde
coordinates: lat: 16.696
lon: -22.982
Younger residents of Beijing have become more attracted to the nightlife, which has flourished in recent decades, breaking prior cultural traditions that had practically restricted it to the upper class. Today, Houhai, Sanlitun and Wudaokou are Beijing's nightlife hotspots. In 2012 Beijing was named as City of Design and became part of the UNESCO Creative Cities Network. Places of interest.

Geographic entities mentioned:
surface_form: Houhai
instance_of: Lake
countries: People's Republic of China
coordinates: lat: 39.941111111111
lon: 116.37888888889
Yearly sacrifices to the God of Heaven () at the Temple of Heaven have been resumed by Confucian groups in the 2010s. There are temples dedicated to the worship of the Goddess () in the city, one of them near the Olympic Village, and they revolve around a major cult center at Mount Miaofeng.

Geographic entities mentioned:
surface_form: Mount Miaofeng
instance_of: Mountain
countries: People's Republic of China
coordinates: lat: 40.07243
lon: 116.01419
Crow Indian Lake. Crow Indian Lake is a lake in Alberta, Canada. Crow Indian Lake takes its name from the Crow Nation.

Geographic entities mentioned:
surface_form: crow indian lake
instance_of: Lake
countries: Canada
coordinates: lat: 49.36972
lon: -111.78417
Isawa River. The is a river in Iwate Prefecture, Japan. For about half its length it marks the border between Kanegasaki Town and Ōshū City. The river's origin is in the Ōu Mountains just west of Mt. Yakeishi (1548 meters). At its highest point it is called the and flows south until it crosses National Route 397. There it turns west and follows 397 until it is stopped by the Ishibuchi Dam.

Geographic entities mentioned:
surface_form: Mt. Yakeishi
instance_of: Mountain
countries: Japan
coordinates: lat: 39.16361111111111
lon: 140.82888888888888
The Nanda Devi Plutonium Mission was a joint operation by the United States Central Intelligence Agency (CIA) and the Indian Intelligence Bureau (IB) to spy on the nuclear developments being conducted in the Xinjiang Province of China. The agencies cooperated in October 1965 to install a nuclear-powered remote sensing station on the peak of Nanda Devi in the Uttarakhand Garhwal Himalayas.

Geographic entities mentioned:
surface_form: Nanda Devi
instance_of: Mountain
countries: India
coordinates: lat: 30.37388888888889
lon: 79.97083333333333
The Vietnam War was ramping up and the United States had no intelligence data to counter any Chinese threat. The Chinese were conducting nuclear tests in secretive facilities. Two years prior, a top US air force officer led a successful expedition to the summit of Mount Everest. He suggested that the Pentagon should recruit the hardy Sherpas to install a remote sensing station on the summit.

Geographic entities mentioned:
surface_form: Mount Everest
instance_of: Mountain
countries: Nepal
People's Republic of China
coordinates: lat: 27.988055555555555
lon: 86.925
He suggested that the Pentagon should recruit the hardy Sherpas to install a remote sensing station on the summit. But this idea ran into some problem as Mount Everest also bordered China. After consultations with the Indian authorities, the Pentagon arrived at a plan to install a remote sensing station on the summit of Nanda Devi within Indian territory at an altitude of.

Geographic entities mentioned:
surface_form: Mount Everest
instance_of: Mountain
countries: Nepal
People's Republic of China
coordinates: lat: 27.988055555555555
lon: 86.925
He suggested that the Pentagon should recruit the hardy Sherpas to install a remote sensing station on the summit. But this idea ran into some problem as Mount Everest also bordered China. After consultations with the Indian authorities, the Pentagon arrived at a plan to install a remote sensing station on the summit of Nanda Devi within Indian territory at an altitude of.

Geographic entities mentioned:
surface_form: Nanda Devi
instance_of: Mountain
countries: India
coordinates: lat: 30.37388888888889
lon: 79.97083333333333
several of them had been members of the 1963 American Mount Everest expedition along with Bishop: Lute Jerstad, Barry Prather, Barry Corbet and Dave Dingman, the other three were Tom Frost, Robert Schaller and Sandy Bill. Bishop himself wasn't part of the team on the mountain but he was one of the people who met the Indian team when they travelled to the US for training on Denali in summer 1965.

Geographic entities mentioned:
surface_form: Denali
instance_of: Mountain
countries: United States
coordinates: lat: 63.06916666666667
lon: -151.0063888888889
Initial timeline. In July 1965 Kohli and the team members from India flew to the US to undertake training and familiarisation on Denali. They returned to India in August and by mid-September 1965 they were at the base-camp on Nanda Devi with the American climbers Lute Jerstad, Tom Frost and Sandy Bill (Schaller had to pull out due to an injury).

Geographic entities mentioned:
surface_form: Denali
instance_of: Mountain
countries: United States
coordinates: lat: 63.06916666666667
lon: -151.0063888888889
Two ascents of Nanda Devi were made during the search operation. On 8th June Gurcharan Bhangu reached the summit with Sherpa Tashi and on 20 August Rob Schaller made a solo ascent of
Nanda Kot. In the light of the problems which had arisen when attempting to install the equipment on Nanda Devi, an alterntive plan was devised which involved placing a device on the nearby Nanda Kot.

Geographic entities mentioned:
surface_form: Nanda Kot
instance_of: Mountain
countries: India
coordinates: lat: 30.281666666667
lon: 80.068333333333
Its larvae ate the roots, rhizomes, and the buds. As the plant died, it turned brown and sank to the bottom of the waterway and decomposed. This weevil was used with success in other parts of the world (13 tropical countries) such as the Sepik River in Papua, Sri Lanka, Lake Ossa in Cameroon as part of an AMMCO project to restore African manatee; Wappa Dam in Queensland, and lagoons (e.g.

Geographic entities mentioned:
surface_form: Lake Ossa
instance_of: Lake
countries: Cameroon
coordinates: lat: 3.7966638888889
lon: 10.024777777778
New York and Canada Railroad. The New York and Canada Railroad was a railway company that operated in the state of New York between 1873 and 1908. It was established to consolidate existing companies in the northern part of the state and to complete a north–south railway line along the west side of Lake Champlain.

Geographic entities mentioned:
surface_form: Lake Champlain
instance_of: Lake
countries: United States
Canada
coordinates: lat: 44.53
lon: -73.33
History. The backers of the Whitehall and Plattsburgh Railroad had attempted to establish a railway line along the west side of Lake Champlain via the Ausable River valley. The effort sputtered out in 1870–1871, leaving two disconnected railway lines: a line between Plattsburgh, New York, and Ausable, New York, and a line between Port Henry, New York, and Fort Ticonderoga.

Geographic entities mentioned:
surface_form: Lake Champlain
instance_of: Lake
countries: United States
Canada
coordinates: lat: 44.53
lon: -73.33
Junk Bay Chinese Permanent Cemetery is built on the east side of Chiu Keng Wan Shan. Access. Parts of Wilson Trail Section 3 is built along the foot of Chiu Keng Wan Shan on the west side. It is possible to access the summit of Chiu Keng Wan Shan after walking up from O King Road, which is a road that runs between Chiu Keng Wan Shan and nearby Black Hill.

Geographic entities mentioned:
surface_form: Black Hill
instance_of: Mountain
countries: People's Republic of China
coordinates: lat: 22.3091737
lon: 114.2441792
There was a water aerodrome at Fancy Lake. French explorer Samuel de Champlain is said to have arrived in the area in 1604, mapped the offshore islands, and gave the river its name after landing near the mouth. The river lends its name to the small community of Petite Riviere, which was at one time known as Petite Riviere Bridge.

Geographic entities mentioned:
surface_form: petite riviere
instance_of: Watercourse
countries: Canada
coordinates: lat: 44.226597
lon: -64.434607
surface_form: petite riviere
instance_of: Watercourse
countries: Canada
coordinates: lat: 44.226597
lon: -64.434607
Petite Rivière (Lunenburg County). Petite Rivière is a river in Nova Scotia, Canada entirely within Lunenburg County. It is fed by numerous lakes, and a portion of the watershed is the drinking water supply for the town of Bridgewater. Three of the lakes on Petite Rivière (Hebb, Millipisigate, and Minamkeak) are the only known habitat of the Atlantic Whitefish.

Geographic entities mentioned:
surface_form: petite rivière
instance_of: Watercourse
countries: Canada
coordinates: lat: 44.226597
lon: -64.434607
It is fed by numerous lakes, and a portion of the watershed is the drinking water supply for the town of Bridgewater. Three of the lakes on Petite Rivière (Hebb, Millipisigate, and Minamkeak) are the only known habitat of the Atlantic Whitefish. Through damming of the lakes, some of the water that once fed the Medway River now flows through the Petite Rivière system.

Geographic entities mentioned:
surface_form: petite rivière
instance_of: Watercourse
countries: Canada
coordinates: lat: 44.226597
lon: -64.434607
Three of the lakes on Petite Rivière (Hebb, Millipisigate, and Minamkeak) are the only known habitat of the Atlantic Whitefish. Through damming of the lakes, some of the water that once fed the Medway River now flows through the Petite Rivière system. There was a water aerodrome at Fancy Lake.

Geographic entities mentioned:
surface_form: petite rivière
instance_of: Watercourse
countries: Canada
coordinates: lat: 44.226597
lon: -64.434607
Samanjac. Samanjac (Serbian Cyrillic: Самањац) is a mountain in central Serbia, near the town of Boljevac. Its highest peak has an elevation of 853 meters above sea level.

Geographic entities mentioned:
surface_form: samanjac
instance_of: Mountain
countries: Serbia
coordinates: lat: 43.79472222
lon: 21.68083333
Islands that form part of the arc are the Eastern Coastal Range of Taiwan, Green Island, Taiwan, Orchid Island, Kaotai Rock, Mavudis or Y'ami Island, Mabudis, Siayan Island, Itbayat Island, Diogo Island, Batan Island, Unnamed volcano Ibuhos, Sabtang Island, Babuyan, Didicas, and Camiguin de Babuyanes. At the south end it terminates on Luzon.

Geographic entities mentioned:
surface_form: Camiguin de Babuyanes
instance_of: Mountain
countries: Philippines
coordinates: lat: 18.833611111111
lon: 121.86111111111
Corelli Horn. Corelli Horn () is a prominent rocky pinnacle with a distinctive pointed summit, high, standing west of the north end of the LeMay Range in central Alexander Island, Antarctica. It was first mapped in 1960 by D. Searle of the Falkland Islands Dependencies Survey, from air photos obtained by the Ronne Antarctic Research Expedition in 1947–48.

Geographic entities mentioned:
surface_form: corelli horn
instance_of: Mountain
coordinates: lat: -70.7
lon: -69.8167
Corelli Horn. Corelli Horn () is a prominent rocky pinnacle with a distinctive pointed summit, high, standing west of the north end of the LeMay Range in central Alexander Island, Antarctica. It was first mapped in 1960 by D. Searle of the Falkland Islands Dependencies Survey, from air photos obtained by the Ronne Antarctic Research Expedition in 1947–48.

Geographic entities mentioned:
surface_form: corelli horn
instance_of: Mountain
coordinates: lat: -70.7
lon: -69.8167
surface_form: alexander
instance_of: Mountain
coordinates: lat: -63.3039
lon: -55.80564
Corelli Horn. Corelli Horn () is a prominent rocky pinnacle with a distinctive pointed summit, high, standing west of the north end of the LeMay Range in central Alexander Island, Antarctica. It was first mapped in 1960 by D. Searle of the Falkland Islands Dependencies Survey, from air photos obtained by the Ronne Antarctic Research Expedition in 1947–48.

Geographic entities mentioned:
surface_form: searle
instance_of: Mountain
coordinates: lat: -67.81666667
lon: -67.25
The last large jökulhlaup was due to an explosive eruption of the Katla volcano under the glacier in 1918, and the water volume at the peak of the jökulhlaup was estimated to be around 200,000 - 300,000 m³/s. History of settlements. South of the road rises Hjörleifshöfði to a height of. The mountain is named after Hjörleifr Hróðmarsson.

Geographic entities mentioned:
surface_form: Hjörleifshöfði
instance_of: Mountain
countries: Iceland
coordinates: lat: 63.41666667
lon: -18.76666667
2011–2012 Puyehue-Cordón Caulle eruption. The 2011–2012 Puyehue-Cordón Caulle eruption () was a volcanic eruption that began in the Puyehue-Cordón Caulle volcanic complex in Chile on 4 June 2011. The eruption, which occurred from the Cordón Caulle fissure after 51 years of the volcano being inactive, is one of the largest volcanic eruptions of the 21st century thus far.

Geographic entities mentioned:
surface_form: Puyehue-Cordón Caulle
instance_of: Mountain
countries: Chile
coordinates: lat: -40.59027777777778
lon: -72.11722222222222
The cattle economy was also damaged. Scientists from the Southern University of Chile analyzed waters from the Nilahue and Golgol rivers, the two principal collectors of waters from Cordón Caulle. Scientists found that if solid particles were removed the water was safe to drink.

Geographic entities mentioned:
surface_form: Golgol
instance_of: Watercourse
countries: Chile
coordinates: lat: -40.676388888889
lon: -72.340277777778
Scientists found that if solid particles were removed the water was safe to drink. Although very little ash was deposited on the western side of the volcano, the ash reached Puyehue Lake through river transport, depositing a layer of tephra at the bottom of the lake. Livestock.

Geographic entities mentioned:
surface_form: Puyehue Lake
instance_of: Lake
countries: Chile
coordinates: lat: -40.683333333333
lon: -72.45
On the ground lava, ash and volcanic stone can impede vehicle movement. Chile. Initially, because of the wind direction (to east), the flights within Chile were not interrupted and only the highway Route 215-CH and the &quot;Cardenal Samore Pass&quot; was reported to be covered by 10 to 15 cm of &quot;volcanic stone&quot; by Chilean authorities. and closed down on 4 June.

Geographic entities mentioned:
surface_form: &quot;Cardenal Samore Pass&quot;
instance_of: Mountain
countries: Chile
Argentina
coordinates: lat: -40.713175
lon: -71.944027
and closed down on 4 June. The Chilean government increased the frequency of barges on the Pirihueico Lake in Huahum Pass to transport passengers traveling between Chile and Argentina. Huahum Pass is approximately 100 km north of the closed &quot;Cardenal Samore Pass&quot;.

Geographic entities mentioned:
surface_form: Pirihueico Lake
instance_of: Lake
countries: Chile
coordinates: lat: -39.93
lon: -71.790277777778
Mission Valley, San Diego. Mission Valley is a wide river valley trending east–west in San Diego, California, United States, through which the San Diego River flows to the Pacific Ocean. For planning purposes the City of San Diego divides it into two neighborhoods: Mission Valley East and Mission Valley West'&quot;.

Geographic entities mentioned:
surface_form: mission valley, san diego
instance_of: Valley
countries: United States
coordinates: lat: 32.767261111111
lon: -117.14961666667
Mission Valley, San Diego. Mission Valley is a wide river valley trending east–west in San Diego, California, United States, through which the San Diego River flows to the Pacific Ocean. For planning purposes the City of San Diego divides it into two neighborhoods: Mission Valley East and Mission Valley West'&quot;.

Geographic entities mentioned:
surface_form: mission valley
instance_of: Valley
countries: United States
coordinates: lat: 32.767261111111
lon: -117.14961666667
surface_form: river valley
instance_of: Valley
countries: United States
coordinates: lat: 35.36
lon: -93.37
Mission Valley is a wide river valley trending east–west in San Diego, California, United States, through which the San Diego River flows to the Pacific Ocean. For planning purposes the City of San Diego divides it into two neighborhoods: Mission Valley East and Mission Valley West'&quot;. Mission Valley was the site of the first Spanish settlement in California, established in 1769.

Geographic entities mentioned:
surface_form: mission valley
instance_of: Valley
countries: United States
coordinates: lat: 32.767261111111
lon: -117.14961666667
surface_form: mission valley
instance_of: Valley
countries: United States
coordinates: lat: 32.767261111111
lon: -117.14961666667
surface_form: mission valley
instance_of: Valley
countries: United States
coordinates: lat: 32.767261111111
lon: -117.14961666667
Cañada in Spanish means gully, ravine, or glen. The name was changed to Mission Valley in the 1860s in reference to Mission San Diego de Alcalá. The Mission Valley area was inhabited by Kumeyaay Indians for more than 10,000 years, which was home to many Kumeyaay villages such as the villages of Nipaquay (&quot;Nipawai&quot;), Haiir, and Cosoy (&quot;Kosa'aay&quot;).

Geographic entities mentioned:
surface_form: mission valley
instance_of: Valley
countries: United States
coordinates: lat: 32.767261111111
lon: -117.14961666667
The first Spanish settlement in present-day California was the Presidio of San Diego and Mission San Diego de Alcalá, both established in 1769 next to the village of Cosoy. The Presidio and Mission were located at the western end of Mission Valley, which is now present-day Old Town, where the valley opens out into the flood plain of the San Diego River.

Geographic entities mentioned:
surface_form: mission valley
instance_of: Valley
countries: United States
coordinates: lat: 32.767261111111
lon: -117.14961666667
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 34.155833333333334
lon: -118.28777777777778
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 61.3833
lon: -150.25
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 47.7174
lon: -117.047423
The Presidio and Mission were located at the western end of Mission Valley, which is now present-day Old Town, where the valley opens out into the flood plain of the San Diego River. In 1774, the Mission was moved to its present location at the eastern end of Mission Valley because of better access to freshwater for drinking and farming.

Geographic entities mentioned:
surface_form: mission valley
instance_of: Valley
countries: United States
coordinates: lat: 32.767261111111
lon: -117.14961666667
surface_form: mission valley
instance_of: Valley
countries: United States
coordinates: lat: 32.767261111111
lon: -117.14961666667
After World War II, the city's expansion began to encroach on the valley. The last of the valley's dairy farms closed in the early 1960s. Another early activity in Mission Valley was quarrying sand and gravel from its walls. A large quarry on the north side of the valley was in operation for most of the 20th century.

Geographic entities mentioned:
surface_form: mission valley
instance_of: Valley
countries: United States
coordinates: lat: 32.767261111111
lon: -117.14961666667
The development of Mission Valley began in 1953 when the first hotel was built in what is now Hotel Circle. In 1958, the city council rezoned of the river valley to allow the construction of San Diego's first regional shopping center. The Mission Valley Center (now Westfield Mission Valley) opened in 1961 and was followed by several other large regional shopping malls.

Geographic entities mentioned:
surface_form: river valley
instance_of: Valley
countries: United States
coordinates: lat: 35.36
lon: -93.37
In 1958, the city council rezoned of the river valley to allow the construction of San Diego's first regional shopping center. The Mission Valley Center (now Westfield Mission Valley) opened in 1961 and was followed by several other large regional shopping malls. In the late 1950s and early 1960s, the U.S.

Geographic entities mentioned:
surface_form: mission valley
instance_of: Valley
countries: United States
coordinates: lat: 32.767261111111
lon: -117.14961666667
The Mission Valley Center (now Westfield Mission Valley) opened in 1961 and was followed by several other large regional shopping malls. In the late 1950s and early 1960s, the U.S. 80 freeway (now Interstate 8) was constructed through Mission Valley, further opening the area up for development.

Geographic entities mentioned:
surface_form: mission valley
instance_of: Valley
countries: United States
coordinates: lat: 32.767261111111
lon: -117.14961666667
In the late 1950s and early 1960s, the U.S. 80 freeway (now Interstate 8) was constructed through Mission Valley, further opening the area up for development. Westgate Park, a baseball stadium for the then-minor-league San Diego Padres, was built in Mission Valley in 1957.

Geographic entities mentioned:
surface_form: mission valley
instance_of: Valley
countries: United States
coordinates: lat: 32.767261111111
lon: -117.14961666667
San Diego Stadium was demolished in 2021 and was replaced by Snapdragon Stadium in 2022. Boundaries. Mission Valley stretches as far west as Interstate 5 and as far east as Interstate 15. The exact boundary between Mission Valley East and West is State Route 163. Government. Mission Valley is located in City Council District 7 and is currently represented by Councilmember Raul Campillo.

Geographic entities mentioned:
surface_form: mission valley
instance_of: Valley
countries: United States
coordinates: lat: 32.767261111111
lon: -117.14961666667
surface_form: mission valley
instance_of: Valley
countries: United States
coordinates: lat: 32.767261111111
lon: -117.14961666667
Mission Valley serves as a path for Interstate 8 and is crossed at its mouth by Interstate 5. Both I-8 and I-5 serve as the major east-west and north-south routes respectively, for San Diego. At the Jack Schrade Interchange, Interstate 805 crosses Mission Valley and connects with Interstate 8. Interstate 15 and State Route 163 also cross Mission Valley and connect with Interstate 8.

Geographic entities mentioned:
surface_form: mission valley
instance_of: Valley
countries: United States
coordinates: lat: 32.767261111111
lon: -117.14961666667
Both I-8 and I-5 serve as the major east-west and north-south routes respectively, for San Diego. At the Jack Schrade Interchange, Interstate 805 crosses Mission Valley and connects with Interstate 8. Interstate 15 and State Route 163 also cross Mission Valley and connect with Interstate 8. The Green Line of the San Diego Trolley system also runs through Mission Valley.

Geographic entities mentioned:
surface_form: mission valley
instance_of: Valley
countries: United States
coordinates: lat: 32.767261111111
lon: -117.14961666667
At the Jack Schrade Interchange, Interstate 805 crosses Mission Valley and connects with Interstate 8. Interstate 15 and State Route 163 also cross Mission Valley and connect with Interstate 8. The Green Line of the San Diego Trolley system also runs through Mission Valley. The main hub for buses is located at the Fashion Valley Transit Center and Mall.

Geographic entities mentioned:
surface_form: mission valley
instance_of: Valley
countries: United States
coordinates: lat: 32.767261111111
lon: -117.14961666667
The Green Line of the San Diego Trolley system also runs through Mission Valley. The main hub for buses is located at the Fashion Valley Transit Center and Mall. Other trolley stations in the valley are found at Linda Vista, Hazard Center, Mission Valley Center, Rio Vista, Fenton Parkway, and Stadium. Attractions.

Geographic entities mentioned:
surface_form: mission valley
instance_of: Valley
countries: United States
coordinates: lat: 32.767261111111
lon: -117.14961666667
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 34.155833333333334
lon: -118.28777777777778
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 61.3833
lon: -150.25
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 47.7174
lon: -117.047423
Other trolley stations in the valley are found at Linda Vista, Hazard Center, Mission Valley Center, Rio Vista, Fenton Parkway, and Stadium. Attractions. Toward the eastern end of Mission Valley lies Mission San Diego de Alcalá, for which the valley is named. At the southwestern end overlooking the valley is Presidio Park.

Geographic entities mentioned:
surface_form: mission valley
instance_of: Valley
countries: United States
coordinates: lat: 32.767261111111
lon: -117.14961666667
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 34.155833333333334
lon: -118.28777777777778
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 61.3833
lon: -150.25
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 47.7174
lon: -117.047423
All three attractions are listed on the National Register of Historic Places. Three major shopping malls located in Mission Valley are Fashion Valley Mall, Hazard Center Mall, and Westfield Mission Valley. Many other commercial developments can be found in the region as well, including smaller shopping plazas, auto malls, and vocational schools.

Geographic entities mentioned:
surface_form: mission valley
instance_of: Valley
countries: United States
coordinates: lat: 32.767261111111
lon: -117.14961666667
surface_form: mission valley
instance_of: Valley
countries: United States
coordinates: lat: 32.767261111111
lon: -117.14961666667
The frontage roads east of Highway 163 are called Camino del Rio North and Camino del Rio South. Recently built Snapdragon Stadium is in Mission Valley East near the I-8/I-15 interchange. At the outlet of Mission Valley lie SeaWorld, Mission Bay, and other San Diego attractions.

Geographic entities mentioned:
surface_form: mission valley
instance_of: Valley
countries: United States
coordinates: lat: 32.767261111111
lon: -117.14961666667
surface_form: mission valley
instance_of: Valley
countries: United States
coordinates: lat: 32.767261111111
lon: -117.14961666667
In 1774, the Mission was moved to its present location at the eastern end of Mission Valley because of better access to freshwater for drinking and farming. Until the 1940s, Mission Valley remained largely undeveloped, featuring dairy farms and other agricultural activities; the city of San Diego was largely confined to areas south of the valley.

Geographic entities mentioned:
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 34.155833333333334
lon: -118.28777777777778
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 61.3833
lon: -150.25
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 47.7174
lon: -117.047423
Until the 1940s, Mission Valley remained largely undeveloped, featuring dairy farms and other agricultural activities; the city of San Diego was largely confined to areas south of the valley. After World War II, the city's expansion began to encroach on the valley. The last of the valley's dairy farms closed in the early 1960s.

Geographic entities mentioned:
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 34.155833333333334
lon: -118.28777777777778
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 34.155833333333334
lon: -118.28777777777778
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 61.3833
lon: -150.25
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 61.3833
lon: -150.25
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 47.7174
lon: -117.047423
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 47.7174
lon: -117.047423
The last of the valley's dairy farms closed in the early 1960s. Another early activity in Mission Valley was quarrying sand and gravel from its walls. A large quarry on the north side of the valley was in operation for most of the 20th century. The quarry ceased operation around 2000 and is now the site of the Civita mixed-use development.

Geographic entities mentioned:
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 34.155833333333334
lon: -118.28777777777778
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 61.3833
lon: -150.25
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 47.7174
lon: -117.047423
Attractions. Toward the eastern end of Mission Valley lies Mission San Diego de Alcalá, for which the valley is named. At the southwestern end overlooking the valley is Presidio Park. At the foot of Presidio Hill lies Old Town San Diego State Historic Park, the original site of the town of San Diego. All three attractions are listed on the National Register of Historic Places.

Geographic entities mentioned:
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 34.155833333333334
lon: -118.28777777777778
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 61.3833
lon: -150.25
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 47.7174
lon: -117.047423
Several condominiums and apartments can also be found in the area. History. The San Diego River valley was originally called Emat Kuseyaay, which was then named by the Spanish as La Cañada de San Diego. Cañada in Spanish means gully, ravine, or glen. The name was changed to Mission Valley in the 1860s in reference to Mission San Diego de Alcalá.

Geographic entities mentioned:
surface_form: river valley
instance_of: Valley
countries: United States
coordinates: lat: 35.36
lon: -93.37
This refers to the membranous bracts or spathes, under the flowers. It was originally described from specimens collected from near to the Caspian Sea. It was first described by Johann Heinrich Friedrich Link and then published by Karl Ludwig Willdenow (using Link's description of the plant), in 'Jahrbücher der Gewächskunde' (of Berlin and Leipzig, Jahrb. Gewächsk.) Vol.1 Issue 3, page 71 in 1820.

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
Seewen, Schwyz. Seewen is a village in the municipality of Schwyz, itself in the canton of Schwyz in Switzerland. It lies some to the west of the town centre of Schwyz, and near the shore of Lake Lauerz. The outfall stream of the lake, the Seeweren, passes through the village on its way to join the Muota river. Schwyz railway station, on the Gotthard railway, is located in Seewen.

Geographic entities mentioned:
surface_form: Lake Lauerz
instance_of: Lake
countries: Switzerland
coordinates: lat: 47.033611111111
lon: 8.6033333333333
Zschonerbach. The Zschonerbach is a small river of Saxony, Germany. It flows into the Elbe near Dresden.

Geographic entities mentioned:
surface_form: Elbe
instance_of: Watercourse
countries: Czech Republic
Germany
coordinates: lat: 53.922222222222224
lon: 8.722222222222221
Between 1863 and the early 1900s, there were numerous territorial changes, including the merger and splitting of states. Thereafter, until the late 1990s, the states were left unchanged. Recent years have seen the creation of three new states: Delta Amacuro, Amazonas, and Vargas (in that order). Municipal organization.

Geographic entities mentioned:
surface_form: Delta Amacuro
instance_of: Body of water
countries: Venezuela
coordinates: lat: 8.7
lon: -61.15
Sgorr Ruadh. Sgorr Ruadh () is a mountain between Strath Carron and Glen Torridon in Wester Ross in the Northwest Highlands of Scotland. It is located in Coire Lair near Achnashellach along with two other mountains, Beinn Liath Mhòr and Fuar Tholl, and is often climbed together with one or both of these other mountains. Geography.

Geographic entities mentioned:
surface_form: Beinn Liath Mhòr
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 57.512083
lon: -5.400618
surface_form: Fuar Tholl
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 57.485376
lon: -5.379188
Sgorr Ruadh. Sgorr Ruadh () is a mountain between Strath Carron and Glen Torridon in Wester Ross in the Northwest Highlands of Scotland. It is located in Coire Lair near Achnashellach along with two other mountains, Beinn Liath Mhòr and Fuar Tholl, and is often climbed together with one or both of these other mountains. Geography.

Geographic entities mentioned:
surface_form: sgorr ruadh
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 57.498622
lon: -5.407747
The centre of the crag is split by a large couloir (gully). There are plenty of easier routes on the crag. Ascents and summit. Direct ascents of Sgorr Ruadh are usually started from Achnashellach in Glen Carron, although it is possible to approach from Glen Torridon on a considerably longer and rougher route.

Geographic entities mentioned:
surface_form: sgorr ruadh
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 57.498622
lon: -5.407747
From Achnnashellach the right of way which goes up Coire Lair to Torridon is taken for two kilometres where a cairn indicates a path bearing left which crosses the River Lair (the river often requires wading) and climbs to the top of the Bhealaich Mhoir, the pass between Sgorr Ruadh and Fuar Tholl.

Geographic entities mentioned:
surface_form: sgorr ruadh
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 57.498622
lon: -5.407747
The two nearby Munros of Beinn Liath Mhòr and Maol Chean-dearg are well seen as are the Torridon mountains to the west. Many walkers will continue to the adjoining Munro of Beinn Liath Mhòr after climbing Sgorr Ruadh, this is not a straightforward walk as there are areas of crags and high rock steps at the foot of the pass between the two mountains.

Geographic entities mentioned:
surface_form: sgorr ruadh
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 57.498622
lon: -5.407747
surface_form: beinn liath mhòr
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 57.512083
lon: -5.400618
From the top of the bhealaich it is a 275-metre climb to the summit by-passing the many buttresses and gullies on the way. The summit cairn stands in a spectacular position on the edge of sheer slopes and gives spectacular all round views. The two nearby Munros of Beinn Liath Mhòr and Maol Chean-dearg are well seen as are the Torridon mountains to the west.

Geographic entities mentioned:
surface_form: beinn liath mhòr
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 57.512083
lon: -5.400618
Coachella Valley (disambiguation). bv8berqpdp1bdv145x74rx17uao0" xml:space="preserve">Coachella Valley is a valley in California, United States.

Geographic entities mentioned:
surface_form: Coachella Valley
instance_of: Valley
countries: United States
coordinates: lat: 33.72
lon: -116.2
Middle Fell. Middle Fell is a hill or fell in the English Lake District. It is a satellite of Seatallan standing above the northern shore of Wastwater. Middle Fell can be climbed from Greendale near the foot of Wastwater, and a fine view of the lake backed by the Wastwater Screes is visible from the summit. Topography.

Geographic entities mentioned:
surface_form: Seatallan
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.46365
lon: -3.3298194444444
surface_form: wastwater
instance_of: Lake
countries: United Kingdom
coordinates: lat: 54.441666666667
lon: -3.2916666666667
Middle Fell can be climbed from Greendale near the foot of Wastwater, and a fine view of the lake backed by the Wastwater Screes is visible from the summit. Topography. The Western Fells occupy a triangular sector of the Lake District, bordered by the River Cocker to the north east and Wasdale to the south east. Westwards the hills diminish toward the coastal plain of Cumberland.

Geographic entities mentioned:
surface_form: Wasdale
instance_of: Valley
countries: United Kingdom
coordinates: lat: 54.425
lon: -3.35
surface_form: the lake
instance_of: Lake
countries: United Kingdom
coordinates: lat: 51.07
lon: -0.62
Westwards the hills diminish toward the coastal plain of Cumberland. At the central hub of the high country are Great Gable and its satellites, while two principal ridges fan out on either flank of Ennerdale, the western fells in effect being a great horseshoe around this long wild valley. Middle Fell is an outlier of the southern arm.

Geographic entities mentioned:
surface_form: Great Gable
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.482
lon: -3.219
surface_form: ennerdale
instance_of: Valley
countries: United Kingdom
Middle Fell is an outlier of the southern arm. The main watershed runs broadly westwards from Great Gable, dividing the headwaters of Ennerdale and Wasdale. Travelling in this direction the principal hills are Kirk Fell, Pillar, Scoat Fell, Haycock and Caw Fell. Haycock sends out a long southern ridge terminating in Seatallan and Seatallan in turn has a south eastern spur. This is Middle Fell.

Geographic entities mentioned:
surface_form: Wasdale
instance_of: Valley
countries: United Kingdom
coordinates: lat: 54.425
lon: -3.35
surface_form: great gable
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.482
lon: -3.219
surface_form: ennerdale
instance_of: Valley
countries: United Kingdom
Middle Fell is an outlier of the southern arm. The main watershed runs broadly westwards from Great Gable, dividing the headwaters of Ennerdale and Wasdale. Travelling in this direction the principal hills are Kirk Fell, Pillar, Scoat Fell, Haycock and Caw Fell. Haycock sends out a long southern ridge terminating in Seatallan and Seatallan in turn has a south eastern spur. This is Middle Fell.

Geographic entities mentioned:
surface_form: Kirk Fell
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.483
lon: -3.242
surface_form: Scoat Fell
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.490038888889
lon: -3.2998
surface_form: Caw Fell
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.486
lon: -3.343
surface_form: haycock
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.4844
lon: -3.32278
surface_form: pillar
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.497
lon: -3.282
Middle Fell is an outlier of the southern arm. The main watershed runs broadly westwards from Great Gable, dividing the headwaters of Ennerdale and Wasdale. Travelling in this direction the principal hills are Kirk Fell, Pillar, Scoat Fell, Haycock and Caw Fell. Haycock sends out a long southern ridge terminating in Seatallan and Seatallan in turn has a south eastern spur. This is Middle Fell.

Geographic entities mentioned:
surface_form: Seatallan
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.46365
lon: -3.3298194444444
surface_form: haycock
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.4844
lon: -3.32278
surface_form: seatallan
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.46365
lon: -3.3298194444444
Summit. The summit cairn is sited on a small rock outcrop, close to the beginning of the ridge-end descent to the south. The view across Wastwater to the screes of Whin Rigg and Illgill Head is excellent. Also in view is the head of Wasdale and the more distant Coniston Fells. Black Combe appears far off to the south west. Ascents.

Geographic entities mentioned:
surface_form: Whin Rigg
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.41945780200143
lon: -3.3093011327319037
surface_form: Illgill Head
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.4327
lon: -3.2825694444444
surface_form: wastwater
instance_of: Lake
countries: United Kingdom
coordinates: lat: 54.441666666667
lon: -3.2916666666667
The view across Wastwater to the screes of Whin Rigg and Illgill Head is excellent. Also in view is the head of Wasdale and the more distant Coniston Fells. Black Combe appears far off to the south west. Ascents. The simplest ascent is via a path up the nose of the ridge, beginning at Greendale.

Geographic entities mentioned:
surface_form: Black Combe
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.256930555556
lon: -3.3293
Also in view is the head of Wasdale and the more distant Coniston Fells. Black Combe appears far off to the south west. Ascents. The simplest ascent is via a path up the nose of the ridge, beginning at Greendale. A longer alternative climbs the beck to Greendale Tarn before doubling back to the summit along the Seatallan ridge. A circular tour can be contrived via Seatallan and Buckbarrow.

Geographic entities mentioned:
surface_form: Buckbarrow
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.442
lon: -3.33514
surface_form: seatallan
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.46365
lon: -3.3298194444444
To the east is Nether Beck, flowing down to the Lake through its long valley. On the other side are the long southern slopes of Red Pike. The southern slopes of Middle Fell fall to the shore of Wastwater, claiming a long section of the northern shore between Nether Beck Bridge and the Greendale road junction. Goat Gill and Smithy Beck provide further drainage on this side.

Geographic entities mentioned:
surface_form: red pike
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.483
lon: -3.29
surface_form: red pike
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.526
lon: -3.3
Middle Fell. Middle Fell is a hill or fell in the English Lake District. It is a satellite of Seatallan standing above the northern shore of Wastwater. Middle Fell can be climbed from Greendale near the foot of Wastwater, and a fine view of the lake backed by the Wastwater Screes is visible from the summit. Topography.

Geographic entities mentioned:
surface_form: middle fell
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.454
lon: -3.311
Middle Fell. Middle Fell is a hill or fell in the English Lake District. It is a satellite of Seatallan standing above the northern shore of Wastwater. Middle Fell can be climbed from Greendale near the foot of Wastwater, and a fine view of the lake backed by the Wastwater Screes is visible from the summit. Topography.

Geographic entities mentioned:
surface_form: middle fell
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.454
lon: -3.311
surface_form: wastwater
instance_of: Lake
countries: United Kingdom
coordinates: lat: 54.441666666667
lon: -3.2916666666667
surface_form: wastwater
instance_of: Lake
countries: United Kingdom
coordinates: lat: 54.441666666667
lon: -3.2916666666667
surface_form: the lake
instance_of: Lake
countries: United Kingdom
coordinates: lat: 51.07
lon: -0.62
At the central hub of the high country are Great Gable and its satellites, while two principal ridges fan out on either flank of Ennerdale, the western fells in effect being a great horseshoe around this long wild valley. Middle Fell is an outlier of the southern arm. The main watershed runs broadly westwards from Great Gable, dividing the headwaters of Ennerdale and Wasdale.

Geographic entities mentioned:
surface_form: middle fell
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.454
lon: -3.311
Travelling in this direction the principal hills are Kirk Fell, Pillar, Scoat Fell, Haycock and Caw Fell. Haycock sends out a long southern ridge terminating in Seatallan and Seatallan in turn has a south eastern spur. This is Middle Fell. Middle Fell begins at the unnamed col on the eastern face of Seatallan at a height of.

Geographic entities mentioned:
surface_form: middle fell
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.454
lon: -3.311