Sarmila/GeoWiki-Features huggingface dataset:
Inspired by the earlier Lehigh & Susquehanna Turnpike, the two toll roads connected Philadelphia and New Jersey (Delaware & Lehigh Valley communities) to Lake Erie at Buffalo, New York via the toll bridge across the Susquehanna River between Berwick and Nescopeck—the &quot;northern terminus&quot; of the Lausanne-Nescopeck Turnpike.

Geographic entities mentioned:
surface_form: Lehigh Valley
instance_of: Valley
countries: United States
coordinates: lat: 40.7
lon: -75.5
surface_form: Lake Erie
instance_of: Lake
countries: Canada
United States
coordinates: lat: 42.25
lon: -80.99972222222222
Via the Lausanne-Nescopeck Turnpike across the river, the turnpike offered a road connecting to the Lehigh River and Lehigh Valley, and after 1818, the Lehigh Canal connecting communities serviced by the road to Allentown, Bethlehem, Easton, and, via the Delaware River or Delaware Canal, Bristol and Philadelphia.

Geographic entities mentioned:
surface_form: Lehigh Valley
instance_of: Valley
countries: United States
coordinates: lat: 40.7
lon: -75.5
The Susquehanna and Tioga Turnpike served as an extension to the Susquehanna and Lehigh Turnpike, whose terminus was at Nescopeck Falls. The turnpike was part of a larger network of turnpikes that formed a path from Philadelphia to Seneca Lake and beyond to Lake Ontario and Niagara. The Susquehanna and Tioga Turnpike was always rough and muddy and contained potholes during the summer.

Geographic entities mentioned:
surface_form: Lake Ontario
instance_of: Lake
countries: Canada
United States
coordinates: lat: 43.72888888888889
lon: -78.10638888888889
Downs Glacier. Downs Glacier is located in Shoshone National Forest, in the U.S. state of Wyoming on the east of the Continental Divide in the Wind River Range. The glacier is south of Downs Mountain and sits at an elevation of between. Downs Glacier is one of many glaciers found in the Fitzpatrick Wilderness, and is part of the largest grouping of glaciers in the American Rocky Mountains.

Geographic entities mentioned:
surface_form: Downs Mountain
instance_of: Mountain
countries: United States
coordinates: lat: 43.31
lon: -109.673
During this period more than 20,000 Turks fled Lebanon, particularly from Beirut, and settled in Germany. Palestinian Turks. Both during and after the 1947–1949 Palestine war, some members of Palestine's Turkish minority fled the region (particularly the Jezreel Valley region and the Golan Heights) and settled in Lebanon, Syria, and Jordan.

Geographic entities mentioned:
surface_form: Jezreel Valley
instance_of: Valley
countries: Israel
coordinates: lat: 32.596388888889
lon: 35.241944444444
Kurri Kurri, New South Wales. Kurri Kurri is a small town in the Hunter Region of New South Wales, Australia, in the Cessnock LGA. At the, its population was 6,174. Kurri Kurri is the largest town in a group of towns and hamlets, including Stanford Merthyr, Pelaw Main, Weston, Abermain and Heddon Greta, called Kurri Kurri - Abermain by the ABS. Its estimated population was 20,631 at the.

Geographic entities mentioned:
surface_form: Hunter Region
instance_of: Valley
countries: Australia
coordinates: lat: -32.56
lon: 151.17083333333332
Queen Elizabeth Range (Antarctica). The Queen Elizabeth Range () is a rugged mountain range that parallels the eastern side of Marsh Glacier for nearly from Nimrod Glacier in the north to Law Glacier in the south. Mount Markham, high, is the highest elevation in the range. Name. The Queen Elizabeth Range was named by J.H.

Geographic entities mentioned:
surface_form: Mount Markham
instance_of: Mountain
coordinates: lat: -82.85
lon: 161.35
Georg Christian Benedict Ackermann. Georg Christian Benedict Ackermann (3 March 1763 – 8 April 1833) was a German theologian and teacher. He was born in Vier (now part of Boizenburg) upon the river Elbe. He visited school in Schwerin in Mecklenburg, then in 1782 the University of Göttingen in Hanover to study theology.

Geographic entities mentioned:
surface_form: Elbe
instance_of: Watercourse
countries: Czech Republic
Germany
coordinates: lat: 53.922222222222224
lon: 8.722222222222221
It was a severe winter that brought starvation to many in the area, but the trading was lucrative and in spring Prescott returned to Fort Snelling with thirty packs of furs. Meanwhile, the Ojibwe members continued on to Leech Lake for the annual maple sugar harvest. At the time of the district's nomination to the National Register in 1973, the exact location of this post had not been rediscovered.

Geographic entities mentioned:
surface_form: Leech Lake
instance_of: Lake
countries: United States
coordinates: lat: 47.166666666667
lon: -94.366666666667
Mount Ryōkami. is a mountain located in the Saitama Prefecture (Chichibu District), at the northern end of the Okuchichibu Mountains.

Geographic entities mentioned:
surface_form: mount ryōkami
instance_of: Mountain
countries: Japan
coordinates: lat: 36.023333
lon: 138.841389
Bengali Language Movement (Barak Valley). The Bengali Language Movement of Barak Valley was a period of protests that began in 1960 against the decision of the Government of Assam to make Assamese the state's sole official language, even though most Barak Valley residents spoke Bengali.

Geographic entities mentioned:
surface_form: Barak Valley
instance_of: Valley
countries: India
coordinates: lat: 24.833333333333332
lon: 92.8
Protest. On 5 February 1961, the Cachar Gana Sangram Parishad was formed to protest the imposition of Assamese in the Bengali-speaking Barak Valley. On 14 April, the people of Silchar, Karimganj, and Hailakandi observed a Sankalpa Divas in protest against the injustice of the Assamese government.

Geographic entities mentioned:
surface_form: Barak Valley
instance_of: Valley
countries: India
coordinates: lat: 24.833333333333332
lon: 92.8
Slate Range (California). The Slate Range is located in the Mojave Desert in San Bernardino County, California, southwest of Death Valley and east of Trona. The mountains lie to the east of Searles Lake and the Argus Range at the southern end of the Panamint Range. The southern part of the range lies in the Naval Air Weapons Station China Lake, which is off-limit to the general public.

Geographic entities mentioned:
surface_form: Death Valley
instance_of: Valley
countries: United States
coordinates: lat: 36.45693888888889
lon: -116.86528055555556
Somers Lake. Somers Lake is a lake located on Vancouver Island south west of the junction of Stamp River and Ash River.

Geographic entities mentioned:
surface_form: island
instance_of: Lake
countries: Canada
coordinates: lat: 53.783333333333
lon: -94.666666666667
surface_form: somers lake
instance_of: Lake
countries: Canada
coordinates: lat: 49.3569
lon: -124.989
Somers Lake. Somers Lake is a lake located on Vancouver Island south west of the junction of Stamp River and Ash River.

Geographic entities mentioned:
surface_form: somers lake
instance_of: Lake
countries: Canada
coordinates: lat: 49.3569
lon: -124.989
This is a list, arranged by region, of films and television series shot in the Lower Mainland, including several prominent filming locations in Greater Vancouver and the Fraser Valley, plus those in the adjoining Sea-to-Sky Corridor and Sunshine Coast regions. The Bridge Studios. See The Bridge Studios article for full listing. Pemberton. See Pemberton for details.

Geographic entities mentioned:
surface_form: Fraser Valley
instance_of: Valley
countries: Canada
coordinates: lat: 49.108333333333
lon: -122.29166666667
Many engines of this type were used to power the SSZ class coastal patrol airships of which 76 were built. Applications. Post war one engine (serial number 332) was fitted into a specially built hull and launched on Windermere in 1922 with the name &quot;Canfly&quot;. With a flywheel added it was directly connected to the boat's propeller without a gearbox.

Geographic entities mentioned:
surface_form: Windermere
instance_of: Lake
countries: United Kingdom
coordinates: lat: 54.358333333333
lon: -2.9361111111111
This fish grows to SL. It was originally described as a subspecies of European chub. &quot;Squalius prespensis&quot; is endemic to the Lake Prespa basin, shared between Albania, Greece, and North Macedonia. It is abundant within its restricted habitat, and seems to have increased in abundance in recent years. However, it is potentially threatened by overfishing, water extraction, and pollution.

Geographic entities mentioned:
surface_form: Lake Prespa
instance_of: Lake
countries: North Macedonia
Albania
Greece
coordinates: lat: 40.9
lon: 21.05
River Isle. The River Isle (also known as the River Ile) flows from its source near Combe St Nicholas, through Somerset, England and discharges into the River Parrett south of Langport near Midelney. Several small springs merge into the river near Wadeford it then flows north past Donyatt, Ilminster, Puckington, and Isle Abbotts, before joining the Parrett.

Geographic entities mentioned:
surface_form: River Parrett
instance_of: Watercourse
countries: United Kingdom
coordinates: lat: 51.2292
lon: -3.00861
House of Veniamin Marinkovic. The house of Veniamin Marinkovic is located in Devići village in Ivanjica. The house of Veniamin Marinkovic is an example of rural architecture in villages that are located at the foot of the mountain of Golija. Today, the monument is enlisted as an immovable cultural property. Veniamin Marinkovic.

Geographic entities mentioned:
surface_form: Golija
instance_of: Mountain
countries: Serbia
coordinates: lat: 43.337777777778
lon: 20.276666666667
It is the former site of a now-closed military base. The lake can be reached by road on Provincial Road 287 from just north of The Pas. Cormorant Lake is in the Saskatchewan River basin and is primarily fed from the northeast from Mitchell Lake and Yawningstone Lake and from the southwest from Clearwater Lake; it exits to the southeast into Moose Lake.

Geographic entities mentioned:
surface_form: clearwater lake
instance_of: Lake
countries: Canada
coordinates: lat: 45.203
lon: -79.233
surface_form: moose lake
instance_of: Lake
countries: Canada
coordinates: lat: 53.94
lon: -100.15
surface_form: mitchell lake
instance_of: Lake
countries: Canada
coordinates: lat: 44.5739
lon: -78.9503
surface_form: moose lake
instance_of: Lake
countries: Canada
coordinates: lat: 52.956944444444446
lon: -118.92027777777778
surface_form: clearwater lake
instance_of: Lake
countries: Canada
coordinates: lat: 52.2667
lon: -120.233
surface_form: moose
instance_of: Watercourse
countries: Canada
coordinates: lat: 52.91444444444444
lon: -118.80638888888889
surface_form: moose lake
instance_of: Lake
countries: Canada
coordinates: lat: 54.251111111111
lon: -110.90694444444
surface_form: cormorant lake
instance_of: Lake
countries: Canada
coordinates: lat: 54.2514
lon: -100.866
surface_form: clearwater lake
instance_of: Lake
countries: Canada
coordinates: lat: 50.8734
lon: -107.9301
surface_form: clearwater lake
instance_of: Lake
countries: Canada
coordinates: lat: 54.05
lon: -101.05
Administratively it is in Division 21, Northern Region of Manitoba, and it lies almost entirely within the Cormorant Provincial Forest. The lake is about wide and long, with a surface area of over. The village of Cormorant is on the east side of the lake, along Via Rail's Winnipeg–Churchill line. The Cormorant Lake Airport is between Cormorant and Dering.

Geographic entities mentioned:
surface_form: winnipeg
instance_of: Lake
countries: Canada
coordinates: lat: 52.116666666667
lon: -97.25
Cormorant Lake (Manitoba). Cormorant Lake is a large lake in northern Manitoba, Canada. Administratively it is in Division 21, Northern Region of Manitoba, and it lies almost entirely within the Cormorant Provincial Forest. The lake is about wide and long, with a surface area of over. The village of Cormorant is on the east side of the lake, along Via Rail's Winnipeg–Churchill line.

Geographic entities mentioned:
surface_form: manitoba
instance_of: Lake
countries: Canada
coordinates: lat: 50.996
lon: -98.762
surface_form: cormorant lake (manitoba)
instance_of: Lake
countries: Canada
coordinates: lat: 54.2514
lon: -100.866
Cormorant Lake (Manitoba). Cormorant Lake is a large lake in northern Manitoba, Canada. Administratively it is in Division 21, Northern Region of Manitoba, and it lies almost entirely within the Cormorant Provincial Forest. The lake is about wide and long, with a surface area of over. The village of Cormorant is on the east side of the lake, along Via Rail's Winnipeg–Churchill line.

Geographic entities mentioned:
surface_form: manitoba
instance_of: Lake
countries: Canada
coordinates: lat: 50.996
lon: -98.762
surface_form: cormorant lake
instance_of: Lake
countries: Canada
coordinates: lat: 54.2514
lon: -100.866
Cormorant Lake (Manitoba). Cormorant Lake is a large lake in northern Manitoba, Canada. Administratively it is in Division 21, Northern Region of Manitoba, and it lies almost entirely within the Cormorant Provincial Forest. The lake is about wide and long, with a surface area of over. The village of Cormorant is on the east side of the lake, along Via Rail's Winnipeg–Churchill line.

Geographic entities mentioned:
surface_form: manitoba
instance_of: Lake
countries: Canada
coordinates: lat: 50.996
lon: -98.762
The lake is about wide and long, with a surface area of over. The village of Cormorant is on the east side of the lake, along Via Rail's Winnipeg–Churchill line. The Cormorant Lake Airport is between Cormorant and Dering. It is the former site of a now-closed military base. The lake can be reached by road on Provincial Road 287 from just north of The Pas.

Geographic entities mentioned:
surface_form: cormorant lake
instance_of: Lake
countries: Canada
coordinates: lat: 54.2514
lon: -100.866
In 1985, Rafty was awarded the Gold Cross of Mount Athos, one of Greece's highest honours, and in 1991 he was awarded the Order of Australia Medal for services to the media. Sir William Dargie, an Australian artist, eight-time winner of the Archibald Prize, and war artist with Rafty in World War II commented: “Tony Rafty is simply splendid.

Geographic entities mentioned:
surface_form: Mount Athos
instance_of: Mountain
countries: Greece
coordinates: lat: 40.15833333333333
lon: 24.327222222222222
Recommendations. The commission rejected the constitution of the boroughs of Rhondda and Wrexham as county boroughs. The proposals set out in the report were not accepted by the government, and, following the establishment of an inter-departmental working group in 1965, a white paper was issued in 1967. This incorporated some of the 1963 proposals and included some innovations.

Geographic entities mentioned:
surface_form: Rhondda
instance_of: Valley
countries: United Kingdom
coordinates: lat: 51.615938888889
lon: -3.4175222222222
Putty Road. (The) Putty Road is a -long rural road that links the Hunter Region in New South Wales to Wilberforce, just north of Windsor on the far northwestern suburban edge of Sydney, Australia. Route.

Geographic entities mentioned:
surface_form: Hunter Region
instance_of: Valley
countries: Australia
coordinates: lat: -32.56
lon: 151.17083333333332
Aruba Dam was built in 1952 across the Voi River. The reservoir created by the dam attracts many animals and water birds. Tsavo West National Park is more mountainous and wetter, with swamps, Lake Jipe and the Mzima Springs. It is known for birdlife and for its large mammals. It is also home to a black rhino sanctuary. Archaeology and history.

Geographic entities mentioned:
surface_form: Lake Jipe
instance_of: Lake
countries: Tanzania
Kenya
coordinates: lat: -3.6069444444444
lon: 37.761666666667
surface_form: Mzima Springs
instance_of: Lake
countries: Kenya
coordinates: lat: -2.98333333
lon: 38.02166667
Two Tsavo Man-Eaters terrorised the construction crews led by John Henry Patterson who eventually shot the pair but not before they had killed one hundred and thirty five Indians and local workers. The railway was eventually completed through to Kisumu on Lake Victoria. Tsavo remained the homeland for Orma pastoralists and Watha hunter-gatherers until 1948, when it was gazetted a national park.

Geographic entities mentioned:
surface_form: Lake Victoria
instance_of: Lake
countries: Tanzania
Uganda
Kenya
coordinates: lat: -1
lon: 33
Swinton Creek Volcano. The Swinton Creek Volcano is an eroded volcanic outcrop in northwestern British Columbia, Canada. It is one of the volcanoes of the Northern Cordilleran Volcanic Province and last erupted in the Pleistocene period.

Geographic entities mentioned:
surface_form: Northern Cordilleran Volcanic Province
instance_of: Mountain
countries: Canada
coordinates: lat: 57.7156
lon: -130.634
Swinton Creek Volcano. The Swinton Creek Volcano is an eroded volcanic outcrop in northwestern British Columbia, Canada. It is one of the volcanoes of the Northern Cordilleran Volcanic Province and last erupted in the Pleistocene period.

Geographic entities mentioned:
surface_form: swinton creek volcano
instance_of: Mountain
countries: Canada
coordinates: lat: 58.57
lon: -129.84
Swinton Creek Volcano. The Swinton Creek Volcano is an eroded volcanic outcrop in northwestern British Columbia, Canada. It is one of the volcanoes of the Northern Cordilleran Volcanic Province and last erupted in the Pleistocene period.

Geographic entities mentioned:
surface_form: swinton creek volcano
instance_of: Mountain
countries: Canada
coordinates: lat: 58.57
lon: -129.84
surface_form: columbia
instance_of: Mountain
countries: Canada
coordinates: lat: 52.1475
lon: -117.44055555555556
The most famous temple of the divine mountain, Myōgi Shrine (妙義神社), is located on Hakuun-zan, on the east slope of Mount Myōgi. During Edo period, people thought that the god of the mountain protected the population from fire and lightnings. Mount Fuji is located south of Mount Myōgi. Mount Myōgi is made out of volcanic rocks (dacite, tuff) and conglomerates.

Geographic entities mentioned:
surface_form: Mount Fuji
instance_of: Mountain
countries: Japan
coordinates: lat: 35.36055555555556
lon: 138.7275
It is also featured on the 'mo' card in Jomo Karuta. Overview. Mount Myōgi is composed of many different peaks: Hakuun-zan (白雲山), Kondō-san (金洞山), Kinkei-san (金鶏山), Sōma-dake (相馬岳), Mitake-san (御岳山), Chōsunokashira (丁須ノ頭), Yakyu-san (谷急山) and others. Mount Myōgi is generally separated in its south side (known as the front side) and its north side (known as the back side).

Geographic entities mentioned:
surface_form: mitake
instance_of: Mountain
countries: Japan
coordinates: lat: 35.78333333
lon: 139.15
surface_form: kinkei-san
instance_of: Mountain
countries: Japan
coordinates: lat: 38.9933
lon: 141.109
surface_form: mount myōgi
instance_of: Mountain
countries: Japan
coordinates: lat: 36.298611111111
lon: 138.73472222222
Mount Myōgi is generally separated in its south side (known as the front side) and its north side (known as the back side). For instance, when looking at Kinkei-san from Shimonita, the mount is referred to as Nakano-take (中之嶽). Among the many peaks of Mount Myōgi, which is already considered having a picturesque form, the landscape of Nakano-take is very particular.

Geographic entities mentioned:
surface_form: kinkei-san
instance_of: Mountain
countries: Japan
coordinates: lat: 38.9933
lon: 141.109
Mount Myōgi. is one of the major mountains in Gunma Prefecture, Japan. Its straddles the border between the municipalities of Annaka, Shimonita and Tomioka. Well known for its rocks weathered into fantastic forms, this famous peak is ranked among Japan's three most noted places of rugged beauty. There are many hiking courses, and when the foliage changes color there are splendid views to be seen.

Geographic entities mentioned:
surface_form: mount myōgi
instance_of: Mountain
countries: Japan
coordinates: lat: 36.298611111111
lon: 138.73472222222
The highest point is the peak of the Mt. Sōmadake (相馬岳) reaching. It is also a National Place of Scenic Beauty as determined by the Agency for Cultural Affairs in Japan in 1923. Mount Myōgi, along with Mount Akagi and Mount Haruna, is one of the &quot;Three Mountains of Jōmō&quot;. (Jōmō is an old name for Gunma.). It is also featured on the 'mo' card in Jomo Karuta. Overview.

Geographic entities mentioned:
surface_form: mount myōgi
instance_of: Mountain
countries: Japan
coordinates: lat: 36.298611111111
lon: 138.73472222222
Mount Myōgi is generally separated in its south side (known as the front side) and its north side (known as the back side). For instance, when looking at Kinkei-san from Shimonita, the mount is referred to as Nakano-take (中之嶽). Among the many peaks of Mount Myōgi, which is already considered having a picturesque form, the landscape of Nakano-take is very particular.

Geographic entities mentioned:
surface_form: mount myōgi
instance_of: Mountain
countries: Japan
coordinates: lat: 36.298611111111
lon: 138.73472222222
The starting point of the hiking course going through those rocks is Nakano-dake shrine (中之嶽神社). The most famous temple of the divine mountain, Myōgi Shrine (妙義神社), is located on Hakuun-zan, on the east slope of Mount Myōgi. During Edo period, people thought that the god of the mountain protected the population from fire and lightnings. Mount Fuji is located south of Mount Myōgi.

Geographic entities mentioned:
surface_form: mount myōgi
instance_of: Mountain
countries: Japan
coordinates: lat: 36.298611111111
lon: 138.73472222222
To the north is the east-west valley containing the abandoned village of Tyneham and the village of Steeple. On the far side of the valley is the main ridge of the Purbeck Hills rising to Povington Hill (191 m, NNW) and Ridgeway Hill (199m, NE). Much of the surrounding terrain is downland and rough pasture with small woods and copses in the valleys and on the hillsides.

Geographic entities mentioned:
surface_form: Povington Hill
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 50.6297
lon: -2.1597
Hini. Hini is a village in the Boumerdès Province in Kabylie, Algeria. Location. The village is surrounded by Isser River and the town of Ammal in the &quot;Khachna&quot; mountain range.

Geographic entities mentioned:
surface_form: Isser River
instance_of: Watercourse
countries: Algeria
France
coordinates: lat: 36.8391
lon: 3.6679
On the south the U.S.S.R. was bordered by North Korea, Mongolia, China, Afghanistan, Iran, and Turkey. On the southern frontier there were three seas: the Caspian Sea, the world's largest inland sea, as well as the almost completely landlocked Black Sea and Sea of Azov. Romania, Hungary, Czechoslovakia, Poland, Finland, and Norway lay to the west. Topography and drainage.

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
Alpine terrain. Truly alpine terrain was found in the southern mountain ranges. Between the Black and Caspian seas, for example, the Caucasus Mountains rose to impressive heights, marking a continuation of the boundary separating Europe from Asia. One of the peaks, Mount Elbrus, is the highest point in Europe at 5,642 meters.

Geographic entities mentioned:
surface_form: Mount Elbrus
instance_of: Mountain
countries: Russia
Soviet Union
Russian Empire
coordinates: lat: 43.35254
lon: 42.437875
This range, extending to the northwest as the Crimean and Carpathian mountains and to the southeast as the Tien Shan and Pamirs, formed an imposing natural barrier between the Soviet Union and its neighbors to the south. The highest point in the Soviet Union, at 7,495 meters, was Mount Communism (Pik Kommunizma) in the Pamirs near the border with Afghanistan, Pakistan, and China.

Geographic entities mentioned:
surface_form: Mount Communism
instance_of: Mountain
countries: Tajikistan
coordinates: lat: 38.942732
lon: 72.015347
The Soviet Union's four million inland bodies of water chiefly resulted from extensive glaciation. Most prominently they included the Caspian Sea, the world's largest inland sea, and Lake Baikal, the world's deepest and most capacious freshwater lake. Lake Baikal alone held 85 percent of the freshwater resources of the lakes in the Soviet Union and 20 percent of the world's total.

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
surface_form: Lake Baikal
instance_of: Lake
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 53.30277778
lon: 108.00472222
A large scheme to divert the northern rivers southward had been counted on to replenish these seas, but for both economic and environmental reasons, the project was canceled in 1986. Without this diversion project, the Aral Sea, once a body of water larger than any of the Great Lakes except Lake Superior, seemed destined to become the world's largest salt flat as early as the year 2010.

Geographic entities mentioned:
surface_form: Aral Sea
instance_of: Lake
countries: Kazakhstan
Uzbekistan
Russian Empire
Soviet Union
coordinates: lat: 45
lon: 60
surface_form: Lake Superior
instance_of: Lake
countries: Canada
United States
coordinates: lat: 47.52881611111111
lon: -87.76002194444445
Description. Fifty Years of Alaskan Statehood is located in the Fairweather Range of the Saint Elias Mountains. It is set within Glacier Bay National Park and Preserve and is situated northwest of Mount Bertha. Precipitation runoff from the mountain drains to Johns Hopkins Inlet where cruise ships allow views of the peak and the Johns Hopkins Glacier.

Geographic entities mentioned:
surface_form: Mount Bertha
instance_of: Mountain
countries: United States
coordinates: lat: 58.6867
lon: -137.0286
Life. Birx spent his childhood on the combination farm and travelers motel operated by his parents in the small town of Bloomfield in the Finger Lakes Region of New York. Graduating from Bloomfield Central High School in 1959, Birx completed his undergraduate studies at the nearby SUNY Geneseo before moving on to complete his M.A. in anthropology and his Ph.D.

Geographic entities mentioned:
surface_form: Finger Lakes Region
instance_of: Group of lakes
countries: United States
coordinates: lat: 42.666666666667
lon: -76.833333333333
Cedar Township was established in March 1887. Geography. Clark Township is the easternmost township in Mackinac County. It is bordered to the west and northwest by Marquette Township, to the northeast by Chippewa County, and to the south by Lake Huron. According to the U.S. Census Bureau, the township has a total area of, of which are land and (22.27%) are water.

Geographic entities mentioned:
surface_form: Lake Huron
instance_of: Lake
countries: Canada
United States
coordinates: lat: 44.592584
lon: -82.756293
representative. Culberson County is primarily in the Central Time Zone, but northwestern Culberson County, including Guadalupe Mountains National Park, is in the Mountain Time Zone, making it one of only a few U.S. counties officially split into two time zones. It is one of the nine counties that comprise the Trans-Pecos region of West Texas. Native Americans.

Geographic entities mentioned:
surface_form: Trans-Pecos
instance_of: Valley
countries: United States
coordinates: lat: 30.56
lon: -103.79
Geography. According to the United States Census Bureau, the county has a total area of, of which are land and (0.01%) is covered by water. It is the fifth-largest county by area in Texas. The largest part of Guadalupe Mountains National Park lies in the northwestern corner of the county, including McKittrick Canyon and Guadalupe Peak, the highest natural point in Texas at. 2020 census.

Geographic entities mentioned:
surface_form: Guadalupe Peak
instance_of: Mountain
countries: United States
coordinates: lat: 31.891461111111
lon: -104.86071111111
The population was 1,548 at the 2020 census. Geography. According to the United States Census Bureau, the town has a total area of, of which is land and, or 3.10%, is water. The town is located in the northeast Goshen Valley; Santaquin is adjacent to the southeast. The former area of Townsend is located within the southeast area of Genola. Demographics.

Geographic entities mentioned:
surface_form: Goshen Valley
instance_of: Valley
countries: United States
coordinates: lat: 40.093888888889
lon: -111.93
Naushera, Punjab. Nowshera, also &quot;Naushera&quot; (Punjabi and), is a city and Tehsil (administrative subdivisions) in Khushab District, located in the Punjab Province of Pakistan. It is the central hub of the Soon Valley, situated from Khushab city, 62 kilometers from Talagang and from Kallar Kahar and 100km from Sargodha Division.

Geographic entities mentioned:
surface_form: Soon Valley
instance_of: Valley
countries: Pakistan
coordinates: lat: 32.58
lon: 72.15
The best known qazis of this family were Qazi Kalim Allah, Qazi Mian Muhammad Amjad. Qazi Mian Ahmad, Qazi Mazhar Qayyum, Qazi Manzoor ul Haq, Qazi Zafar Hussain. Qazi Mian Muhammad Amjad was born of the qadis family of Naushera, Soon Valley. He was a descendant of Ali Ibn Abi Talib, the fourth caliph of Islam from Al-Abbas ibn Ali.

Geographic entities mentioned:
surface_form: Soon Valley
instance_of: Valley
countries: Pakistan
coordinates: lat: 32.58
lon: 72.15
During the period of British government, he rendered legal opinions on Islamic laws and Fiqh. Raees Azam Naushera, Qazi Mazhar Qayyum was the eldest son of Qazi Mian Muhammad Amjad, and was a well-known &quot;Hakeem&quot; (herbal medicine practitioner), of Soon Valley, and was regarded as an authority on this subject in his time. He died in 1952.

Geographic entities mentioned:
surface_form: Soon Valley
instance_of: Valley
countries: Pakistan
coordinates: lat: 32.58
lon: 72.15
He died in 1952. He was buried in Naushera, Soon Valley
Qazi Manzoor ul Haq, Imam Abu Hanifa of Naushera was the second son of Qazi Mian Muhammad Amjad. He was known as Imam Abu Hanifa of Naushera. He was a scholar of Islamic law. In the age of British government when cases were decided according to English law, Muslims consulted him for his legal opinions on Islamic laws.

Geographic entities mentioned:
surface_form: Soon Valley
instance_of: Valley
countries: Pakistan
coordinates: lat: 32.58
lon: 72.15
degree. He died in 1954 and was buried in Naushera. Khan Sahib Qazi Zafar Hussain, was the third son of Qazi Mian Muhammad Amjad. In 1945, he was awarded by the title of Khan Sahib by the British Government in recognition of his services. He used his family and political influence to help the people of his area. He died in 1968. He was buried in Naushera, Soon Valley.

Geographic entities mentioned:
surface_form: Soon Valley
instance_of: Valley
countries: Pakistan
coordinates: lat: 32.58
lon: 72.15
Just three years after this compromise, Jefferson Davis strongly influenced the Gadsden Purchase to facilitate his preferred southern route which was not viable over the Colorado Plateau. A year after this purchase, Bleeding Kansas began on account of identical thematic tensions.

Geographic entities mentioned:
surface_form: Colorado Plateau
instance_of: Plateau
countries: United States
coordinates: lat: 37
lon: -110
Larvae burrow within the stems and result in substantial damage to the main stem due to tissue necrosis. Likewise, &quot;Cabomba furcata&quot; has become an invasive species in Kerala, India, in the Kalutara district of Sri Lanka, in Chini Lake, Malaysia, and Taiwan. Its presence leads to a decline of water quality and biodiversity.

Geographic entities mentioned:
surface_form: Chini Lake
instance_of: Lake
countries: Malaysia
coordinates: lat: 3.4333333333333
lon: 102.91666666667
Negotiations. The agents employed by the Lord Deputy in the negotiations were Sir William Godolphin and Sir Garrett Moore, an ancestor of the Marquesses of Drogheda. Moore, a personal friend of O'Neill, found him in early March at his retreat near Lough Neagh and persuaded him that he should negotiate peace terms, and would travel under a safe conduct.

Geographic entities mentioned:
surface_form: Lough Neagh
instance_of: Lake
countries: United Kingdom
coordinates: lat: 54.618333333333
lon: -6.3952777777778
They range in depth from to. Kayangan Lake. Accessible by a steep 10-minute climb, the crystal-clear waters of Kayangan Lake are nestled into the mountain walls; underwater is like a moonscape. There's a little wooden walkway and platform to stash your things if you go for a swim.

Geographic entities mentioned:
surface_form: Kayangan Lake
instance_of: Lake
countries: Philippines
coordinates: lat: 11.95726
lon: 120.22623
Homeported in Bayonne, New Jersey, the primary missions of &quot;Penobscot Bay&quot; and her crew are Domestic Icebreaking and Ports, Waterways, & Coastal Security. During the winter months, &quot;Penobscot Bay&quot; is responsible for providing search and rescue capabilities to the ice-covered areas in New York City and the Hudson Valley, as well as throughout coastal New England.

Geographic entities mentioned:
surface_form: Hudson Valley
instance_of: Valley
countries: United States
coordinates: lat: 41.9209
lon: -73.9613
Outline of Wisconsin. Wisconsin &ndash; U.S. state located in the north-central United States and part of the Midwest. It is bordered by Minnesota to the west, Iowa to the southwest, Illinois to the south, Lake Michigan to the east, Upper Michigan to the northeast, and Lake Superior to the north. Wisconsin's capital is Madison, and its largest city is Milwaukee.

Geographic entities mentioned:
surface_form: Lake Michigan
instance_of: Lake
countries: United States
coordinates: lat: 44.007874
lon: -86.756451
surface_form: Lake Superior
instance_of: Lake
countries: Canada
United States
coordinates: lat: 47.52881611111111
lon: -87.76002194444445
Hamilton Fish IV. Hamilton Fish IV or Hamilton Fish Jr. (June 3, 1926 – July 23, 1996) was an American Republican politician who represented parts of New York's Hudson Valley region in the United States House of Representatives for thirteen terms from 1969 to 1995.

Geographic entities mentioned:
surface_form: Hudson Valley
instance_of: Valley
countries: United States
coordinates: lat: 41.9209
lon: -73.9613
Belgrano Lake. Belgrano Lake () is a lake in the Santa Cruz Province of Patagonia, Argentina. It is located in Río Chico Department, in the west of the province. It is located in the Perito Moreno National Park.

Geographic entities mentioned:
surface_form: río chico
instance_of: Watercourse
countries: Argentina
coordinates: lat: -45.612
lon: -68.602
Belgrano Lake. Belgrano Lake () is a lake in the Santa Cruz Province of Patagonia, Argentina. It is located in Río Chico Department, in the west of the province. It is located in the Perito Moreno National Park.

Geographic entities mentioned:
surface_form: belgrano lake
instance_of: Lake
countries: Argentina
coordinates: lat: -47.85111111
lon: -72.14722222
Laguna Seca (Santa Clara County). Laguna Seca (Spanish for &quot;Dry Lake&quot;) is a seasonal lake located in south Santa Clara Valley in the Coyote Valley, an area critical to wildlife as the narrowest corridor connecting Mt. Hamilton and the Diablo Range on the east to the foothills of the Santa Cruz Mountains to the west.

Geographic entities mentioned:
surface_form: Santa Clara Valley
instance_of: Valley
countries: United States
coordinates: lat: 37.366944444444
lon: -121.98388888889
surface_form: dry lake
instance_of: Lake
countries: United States
coordinates: lat: 44.6282988
lon: -97.0561783
surface_form: dry lake
instance_of: Lake
countries: United States
coordinates: lat: 38.3360373
lon: -117.7898285
surface_form: santa clara valley
instance_of: Valley
countries: United States
coordinates: lat: 37.366944444444
lon: -121.98388888889
surface_form: dry lake
instance_of: Lake
countries: United States
coordinates: lat: 45.0425
lon: -97.31972222
surface_form: mt. hamilton
instance_of: Mountain
countries: United States
coordinates: lat: 37.341666666667
lon: -121.64305555556
surface_form: coyote valley
instance_of: Valley
countries: United States
coordinates: lat: 40.3563
lon: -105.859
surface_form: laguna seca
instance_of: Lake
countries: United States
coordinates: lat: 37.2127224
lon: -121.7555049
surface_form: santa clara valley
instance_of: Valley
countries: United States
coordinates: lat: 34.3667
lon: -118.983
Hamilton and the Diablo Range on the east to the foothills of the Santa Cruz Mountains to the west. It is the largest freshwater wetland in Santa Clara County, California and lies between Tulare Hill and the Santa Teresa Hills just west of Santa Teresa Boulevard and north of Bailey Avenue. Laguna Seca is fed by Fisher Creek. A man-made channel extends Fisher Creek to Coyote Creek. History.

Geographic entities mentioned:
surface_form: Tulare Hill
instance_of: Mountain
countries: United States
coordinates: lat: 37.2211
lon: -121.755
surface_form: tulare hill
instance_of: Mountain
countries: United States
coordinates: lat: 37.2211
lon: -121.755
A man-made channel extends Fisher Creek to Coyote Creek. History. The first written historical account of La Laguna Zeca 'the dry lake' was first described on 31 October 1797. Rancho Laguna Seca (Alvires) or Refugio de la Laguna Seca is a Mexican land grant presumably named for the seasonal lake. The grant was made July 22, 1834 to Juan Alvires by Governor José Figueroa.

Geographic entities mentioned:
surface_form: dry lake
instance_of: Lake
countries: United States
coordinates: lat: 44.6282988
lon: -97.0561783
surface_form: dry lake
instance_of: Lake
countries: United States
coordinates: lat: 38.3360373
lon: -117.7898285
surface_form: dry lake
instance_of: Lake
countries: United States
coordinates: lat: 45.0425
lon: -97.31972222
It occasionally dried up in drought years. From 1916 to 1917, Laguna Seca was largely filled in to permit agriculture. Geology and ecology. The remnants of Laguna Seca are bordered by and west of Santa Teresa Boulevard, located at the north end of the area now known as Coyote Valley at the base of the saddle between Tulare Hill and the Santa Teresa Hills.

Geographic entities mentioned:
surface_form: tulare hill
instance_of: Mountain
countries: United States
coordinates: lat: 37.2211
lon: -121.755
surface_form: coyote valley
instance_of: Valley
countries: United States
coordinates: lat: 40.3563
lon: -105.859
surface_form: laguna seca
instance_of: Lake
countries: United States
coordinates: lat: 37.2127224
lon: -121.7555049
In addition, the heavy clay soils characteristic of the bottomland areas, often referred to as &quot;black adobe&quot; soils, often forced groundwater to the surface as springs and seeps. The lake helps recharge the aquifer in the Coyote Valley.

Geographic entities mentioned:
surface_form: coyote valley
instance_of: Valley
countries: United States
coordinates: lat: 40.3563
lon: -105.859
It has been shown that Fisher Creek currently contributes approximately 57% of peak flows that exceed channel holding capacity during a 10-year flooding event at William Street in downtown San Jose and that hydrologic restoration projects designed to spread, capture, and sink excess stormwater in the Coyote Valley could reduce the risk of flooding to downstream areas while also recharging Coyote Valley's groundwater sub-basin (Robins 2016).

Geographic entities mentioned:
surface_form: coyote valley
instance_of: Valley
countries: United States
coordinates: lat: 40.3563
lon: -105.859
surface_form: coyote valley
instance_of: Valley
countries: United States
coordinates: lat: 40.3563
lon: -105.859
Laguna Seca (Santa Clara County). Laguna Seca (Spanish for &quot;Dry Lake&quot;) is a seasonal lake located in south Santa Clara Valley in the Coyote Valley, an area critical to wildlife as the narrowest corridor connecting Mt. Hamilton and the Diablo Range on the east to the foothills of the Santa Cruz Mountains to the west.

Geographic entities mentioned:
surface_form: laguna seca (santa clara county)
instance_of: Lake
countries: United States
coordinates: lat: 37.2127224
lon: -121.7555049
A man-made channel extends Fisher Creek to Coyote Creek. History. The first written historical account of La Laguna Zeca 'the dry lake' was first described on 31 October 1797. Rancho Laguna Seca (Alvires) or Refugio de la Laguna Seca is a Mexican land grant presumably named for the seasonal lake. The grant was made July 22, 1834 to Juan Alvires by Governor José Figueroa.

Geographic entities mentioned:
surface_form: laguna seca
instance_of: Lake
countries: United States
coordinates: lat: 37.2127224
lon: -121.7555049
The grant was made July 22, 1834 to Juan Alvires by Governor José Figueroa. Historically, Laguna Seca was an approximately 1,000-acre spring-fed perennial wetland mosaic of flooded wet meadows and smaller perennial freshwater marshes and lagunas. It occasionally dried up in drought years. From 1916 to 1917, Laguna Seca was largely filled in to permit agriculture. Geology and ecology.

Geographic entities mentioned:
surface_form: laguna seca
instance_of: Lake
countries: United States
coordinates: lat: 37.2127224
lon: -121.7555049
surface_form: lagunas
instance_of: Lake
countries: United States
coordinates: lat: 33.6098638
lon: -117.7574352
The grant was made July 22, 1834 to Juan Alvires by Governor José Figueroa. Historically, Laguna Seca was an approximately 1,000-acre spring-fed perennial wetland mosaic of flooded wet meadows and smaller perennial freshwater marshes and lagunas. It occasionally dried up in drought years. From 1916 to 1917, Laguna Seca was largely filled in to permit agriculture. Geology and ecology.

Geographic entities mentioned:
surface_form: laguna seca
instance_of: Lake
countries: United States
coordinates: lat: 37.2127224
lon: -121.7555049
The lake helps recharge the aquifer in the Coyote Valley. Laguna Seca could provide major flooding protection to downstream San Jose, if the man-made extension of Fisher Creek from Laguna Seca to Coyote Creek was removed.

Geographic entities mentioned:
surface_form: laguna seca
instance_of: Lake
countries: United States
coordinates: lat: 37.2127224
lon: -121.7555049
Today the waters of Laguna Seca are ponded above the surface December to May, but near the surface all year-round. It hosts endangered amphibian species such as the California tiger salamander (&quot;Ambystoma californiense&quot;) and the California red-legged frog (&quot;Rana draytonii&quot;). It is also an important stopover for migrating waterfowl.

Geographic entities mentioned:
surface_form: laguna seca
instance_of: Lake
countries: United States
coordinates: lat: 37.2127224
lon: -121.7555049
It is also an important stopover for migrating waterfowl. Potential restoration of Laguna Seca provides an unusual opportunity to restore natural wetland functions and a diverse, large, natural, valley floor wetland. Successful wetland restoration at Laguna Seca could support a wide range of threatened species, including rare plants, amphibians, and water birds.

Geographic entities mentioned:
surface_form: laguna seca
instance_of: Lake
countries: United States
coordinates: lat: 37.2127224
lon: -121.7555049
The remnants of Laguna Seca are bordered by and west of Santa Teresa Boulevard, located at the north end of the area now known as Coyote Valley at the base of the saddle between Tulare Hill and the Santa Teresa Hills. The marshes and lagunas formed as the bedrock of the Santa Teresa Hills forced groundwater to the surface and drainage was blocked by the natural levees of Coyote Creek.

Geographic entities mentioned:
surface_form: lagunas
instance_of: Lake
countries: United States
coordinates: lat: 33.6098638
lon: -117.7574352
Bland Hollow. Bland Hollow is a valley in Stone County in the U.S. state of Missouri. Bland Hollow has the name of Hiram Bland, a pioneer settler.

Geographic entities mentioned:
surface_form: bland hollow
instance_of: Valley
countries: United States
coordinates: lat: 36.9153354
lon: -93.4968596
Most summit ascents are done either over or around the Lyell Glacier. Seasonal and year-to-year variations on the glacier make it necessary to assess current conditions before choosing a route to the summit. The northwest Ridge, from the saddle between Mount Lyell and nearby Mount Maclure, offers climbing with high snow levels on the glacier.

Geographic entities mentioned:
surface_form: Mount Maclure
instance_of: Mountain
countries: United States
coordinates: lat: 37.7435
lon: -119.282
surface_form: mount lyell
instance_of: Mountain
countries: United States
coordinates: lat: 37.7394
lon: -119.272
Mount Lyell (California). Mount Lyell is the highest point in Yosemite National Park, at. It is located at the southeast end of the Cathedral Range, northwest of Rodgers Peak. The peak as well as nearby Lyell Canyon is named after Charles Lyell, a well-known 19th century geologist. The peak had one of the last remaining glaciers in Yosemite, Lyell Glacier.

Geographic entities mentioned:
surface_form: yosemite
instance_of: Valley
countries: United States
coordinates: lat: 37.721694444444445
lon: -119.646
surface_form: mount lyell
instance_of: Mountain
countries: United States
coordinates: lat: 37.7394
lon: -119.272
It is located at the southeast end of the Cathedral Range, northwest of Rodgers Peak. The peak as well as nearby Lyell Canyon is named after Charles Lyell, a well-known 19th century geologist. The peak had one of the last remaining glaciers in Yosemite, Lyell Glacier. The Lyell Glacier is currently considered to be a permanent ice field, not a living glacier.

Geographic entities mentioned:
surface_form: yosemite
instance_of: Valley
countries: United States
coordinates: lat: 37.721694444444445
lon: -119.646
This rock is very loose and unstable for climbing, making the ascent to the summit plateau dangerous when the glacier is low, exposing the lower reaches of the summit block. For this reason, some climbers consider Mount Lyell and nearby Mount Maclure to actually be geologically part of the Ritter Range.

Geographic entities mentioned:
surface_form: mount maclure
instance_of: Mountain
countries: United States
coordinates: lat: 37.7435
lon: -119.282
surface_form: ritter
instance_of: Mountain
countries: United States
coordinates: lat: 37.6894
lon: -119.199
surface_form: mount lyell
instance_of: Mountain
countries: United States
coordinates: lat: 37.7394
lon: -119.272
Low snow levels increases the grade to class 3 to 4 on the exposed granite ledges, in which cases it may be easier to ascend the glacier more directly to the summit. The summit block of Mount Lyell is composed of dark volcanic granite, similar to its neighbors to the southeast, Rodgers Peak, Mount Davis, Banner Peak, and Mount Ritter.

Geographic entities mentioned:
surface_form: mount davis
instance_of: Mountain
countries: United States
coordinates: lat: 39.7862
lon: -79.1759
surface_form: mount ritter
instance_of: Mountain
countries: United States
coordinates: lat: 37.6894
lon: -119.199
surface_form: ritter
instance_of: Mountain
countries: United States
coordinates: lat: 37.6894
lon: -119.199
surface_form: mount davis
instance_of: Mountain
countries: United States
coordinates: lat: 44.2042
lon: -71.3106
surface_form: mount lyell
instance_of: Mountain
countries: United States
coordinates: lat: 37.7394
lon: -119.272
surface_form: banner peak
instance_of: Mountain
countries: United States
coordinates: lat: 37.6966
lon: -119.195
surface_form: mount davis
instance_of: Mountain
countries: United States
coordinates: lat: 37.7147
lon: -119.22
surface_form: rodgers peak
instance_of: Mountain
countries: United States
coordinates: lat: 37.724971
lon: -119.257506
Mount Lyell (California). Mount Lyell is the highest point in Yosemite National Park, at. It is located at the southeast end of the Cathedral Range, northwest of Rodgers Peak. The peak as well as nearby Lyell Canyon is named after Charles Lyell, a well-known 19th century geologist. The peak had one of the last remaining glaciers in Yosemite, Lyell Glacier.

Geographic entities mentioned:
surface_form: mount lyell (california)
instance_of: Mountain
countries: United States
coordinates: lat: 37.7394
lon: -119.272
The peak had one of the last remaining glaciers in Yosemite, Lyell Glacier. The Lyell Glacier is currently considered to be a permanent ice field, not a living glacier. Mount Lyell divides the Tuolumne River watershed to the north, the Merced to the west, and the Rush Creek drainage in the Mono Lake Basin to the southeast. Climbing.

Geographic entities mentioned:
surface_form: mount lyell
instance_of: Mountain
countries: United States
coordinates: lat: 37.7394
lon: -119.272