Sarmila/GeoWiki-Features huggingface dataset:
Paul, Milwaukee, Detroit, Chicago, and Albany, New York, in the United States. The railway was first built between eastern Canada and British Columbia between 1875 and 1885 (connecting with Ottawa Valley and Georgian Bay area lines built earlier), fulfilling a commitment extended to British Columbia when it entered Confederation in 1871; the CPR was Canada's first transcontinental railway.

Geographic entities mentioned:
surface_form: Ottawa Valley
instance_of: Valley
countries: Canada
coordinates: lat: 45.91682
lon: -77.13276
It then proceeded to Bonfield. It was presumed that the railway would travel through the rich &quot;fertile belt&quot; of the North Saskatchewan River Valley and cross the Rocky Mountains via the Yellowhead Pass. However, a more southerly route across the arid Palliser's Triangle in Saskatchewan and via Kicking Horse Pass and down the Field Hill to the Rocky Mountain Trench was chosen.

Geographic entities mentioned:
surface_form: Rocky Mountain Trench
instance_of: Landform
Valley
countries: Canada
United States
coordinates: lat: 54.5
lon: -122.5
Van Horne, now president of the CPR, asked for government aid, and the government agreed to provide around $3.6 million to construct a railway from Lethbridge, Alberta, through Crowsnest Pass to the south shore of Kootenay Lake, in exchange for the CPR agreeing to reduce freight rates in perpetuity for key commodities shipped in Western Canada.

Geographic entities mentioned:
surface_form: Kootenay Lake
instance_of: Lake
countries: Canada
coordinates: lat: 49.3
lon: -116.75
In 1916, the CPR replaced its line through Rogers Pass, which was prone to avalanches (the most serious of which killed 62 men in 1910) with the Connaught Tunnel, an eight-kilometre-long (5-mile) tunnel under Mount Macdonald that was, at the time of its opening, the longest railway tunnel in the Western Hemisphere.

Geographic entities mentioned:
surface_form: Mount Macdonald
instance_of: Mountain
countries: Canada
coordinates: lat: 51.3083
lon: -117.472
Royal Canadian Pacific. On June 7, 2000, the CPR inaugurated the Royal Canadian Pacific, a luxury excursion service that operates between the months of June and September. It operates along a route from Calgary, through the Columbia Valley in British Columbia, and returning to Calgary via Crowsnest Pass. The trip takes six days and five nights.

Geographic entities mentioned:
surface_form: Columbia Valley
instance_of: Valley
countries: Canada
coordinates: lat: 51.0333
lon: -116.617
This service ended in 1915 when the CPR made an agreement with the Michigan Central to use their Detroit River tunnel opened in 1910. Pennsylvania-Ontario Transportation Company was formed jointly with the PRR in 1906 to operate a ferry across Lake Erie between Ashtabula, Ohio, and Port Burwell, Ontario, to carry freight cars, mostly of coal, much of it to be burned in CPR steam locomotives.

Geographic entities mentioned:
surface_form: Lake Erie
instance_of: Lake
countries: Canada
United States
coordinates: lat: 42.25
lon: -80.99972222222222
CP began a long history of service in the Kootenays region of southern British Columbia beginning with the purchase in 1897 of the Columbia and Kootenay Steam Navigation Company which operated a fleet of steamers and barges on the Arrow Lakes and was merged into the CPR as the CPR Lake and River Service which also served the Arrow Lakes and Columbia River, Kootenay Lake and Kootenai River, Lake Okanagan and Skaha Lake, Slocan Lake, Trout Lake, and Shuswap Lake and the Thompson River/Kamloops Lake.

Geographic entities mentioned:
surface_form: Arrow Lakes
instance_of: Group of lakes
countries: Canada
coordinates: lat: 50
lon: -118
surface_form: Skaha Lake
instance_of: Lake
countries: Canada
coordinates: lat: 49.416666666667
lon: -119.58333333333
surface_form: Slocan Lake
instance_of: Lake
countries: Canada
coordinates: lat: 49.9472
lon: -117.378
surface_form: Shuswap Lake
instance_of: Lake
countries: Canada
coordinates: lat: 51.000693
lon: -119.01263
surface_form: Kamloops Lake
instance_of: Lake
countries: Canada
coordinates: lat: 50.75
lon: -120.66666666666667
He retired from business in 1811 selling his wharves and warehouse complex on the Halifax waterfront to Enos Collins. The following year, he settled on a country estate called Acacia Grove in Starr's Point near Port Williams in Nova Scotia's Annapolis Valley. In 1814, he married Mariah Hammill after the death of his first wife.

Geographic entities mentioned:
surface_form: Annapolis Valley
instance_of: Valley
countries: Canada
coordinates: lat: 44.979166666666664
lon: -64.89222222222222
After the retreating of the main forces he tried to wage his own war in Westphalia (he hoped to provoke an uprising of the local population against the French). But he was defeated, and the units recruited from the prisoners showed themselves poorly. He came to his death swimming over the Elbe, while trying to break an encirclement by Napoleonic troops at Dessau.

Geographic entities mentioned:
surface_form: Elbe
instance_of: Watercourse
countries: Czech Republic
Germany
coordinates: lat: 53.922222222222224
lon: 8.722222222222221
The rear suspension was a custom-made De Dion tube. The tires were mounted on knock-off wire wheels. Wheelbase was, and the track front and rear was. The engine was a Cadillac V8. Motorsports. The C-1 was used in practice at Le Mans, but did not race. In 1951 it appeared at the Mount Equinox hillclimb, where it finished fourth driven by John Fitch.

Geographic entities mentioned:
surface_form: Mount Equinox
instance_of: Mountain
countries: United States
coordinates: lat: 43.1703542
lon: -73.1112166
Aftermath. The next day on September 26, 1861, after the battle of Canada Alamosa was over, the Union cavalry patrol under Captain Robert M. Morris, skirmished with Confederates involved in the Alamosa engagement in the Skirmish near Fort Thorn, New Mexico Territory. This skirmish occurred thirty miles southeast of the town at the north end of Mesilla Valley and 15 miles north of Fort Thorn.

Geographic entities mentioned:
surface_form: Mesilla Valley
instance_of: Valley
countries: United States
coordinates: lat: 31.7903
lon: -106.423
Roads. It is localized on the National Road 43, about from Analavory and from the capital Antananarivo. Nature. The &quot;Ramanavy forest&quot; (Forêt de Ramanavy, or translated: Bats Forest) at from Soavinandriana, that hosts some 20 endemic species of plants. The Lake Itasy, the forth mayor lake of Madagascar, is partly situated in this municipality.

Geographic entities mentioned:
surface_form: Lake Itasy
instance_of: Lake
countries: Madagascar
coordinates: lat: -19.0667
lon: 46.7833
In 798, the Saxons were defeated by the Obodrites, a West Slavic people allied to the Frankish Emperor Charlemagne, at the Battle of Bornhöved (or Schwentine River). A part of the Saxons' land, in Holstein north of the Elbe, was awarded to the Obodrites in 804, as a reward for their victory.

Geographic entities mentioned:
surface_form: Elbe
instance_of: Watercourse
countries: Czech Republic
Germany
coordinates: lat: 53.922222222222224
lon: 8.722222222222221
However, the king's men advised Gudfred against meeting the emperor, and he failed to appear. Charlemagne established a camp at Hollenstedt at the Elbe and sent an errand to Gudfred, asking him to extradite some rebels who had taken refuge in the Danish kingdom. Nothing is known to have come out of this, and the emperor returned to Cologne in September in the same year.

Geographic entities mentioned:
surface_form: Elbe
instance_of: Watercourse
countries: Czech Republic
Germany
coordinates: lat: 53.922222222222224
lon: 8.722222222222221
Both sexes have red eyes, but these are more noticeable in the female than the male. Range and habitat. The phainopepla ranges as far north as central California with the San Joaquin Valley and southern Utah, and south to central Mexico, the interior Mexican Plateau region; the southern edge of the plateau, the transverse mountains is its non-breeding home.

Geographic entities mentioned:
surface_form: San Joaquin Valley
instance_of: Valley
countries: United States
coordinates: lat: 36.628888888889
lon: -120.185
surface_form: Mexican Plateau
instance_of: Plateau
countries: Mexico
coordinates: lat: 24
lon: -103
Some of the stations are still centres of Free Methodist activity today, such as North Chili, New York, site of present-day Roberts Wesleyan College, a Free Methodist school named after the founder. From there fugitive slaves were taken to Lake Ontario and boated across to Canada. Another Underground Railroad site was Pekin, New York, near the Niagara River, where slaves also crossed.

Geographic entities mentioned:
surface_form: Lake Ontario
instance_of: Lake
countries: Canada
United States
coordinates: lat: 43.72888888888889
lon: -78.10638888888889
This tiny town was the site of a Holiness camp meeting, as well, and the site of the organizational conference of the church in 1860. The denomination also has numerous churches in the U.S. Midwest, some of the oldest ones also being in communities that were abolitionist centers and Underground Railroad stops along the southern shore of Lake Michigan.

Geographic entities mentioned:
surface_form: Lake Michigan
instance_of: Lake
countries: United States
coordinates: lat: 44.007874
lon: -86.756451
Vlahina reka. The Vlahina reka () is a river in south-western Bulgaria, a left tributary of the Struma. The river is 27 km long and drains part of the western sections of the Pirin mountain range. The river takes its source from the south-eastern corner of the highest of the five Vlahini Lakes in Northern Pirin at an altitude of 2,302 m to the southwest of Pirin's highest summit Vihren (2,914 m).

Geographic entities mentioned:
surface_form: Vlahini Lakes
instance_of: Group of lakes
countries: Bulgaria
The party was represented in the Regional Council of Friuli-Venezia Giulia from 1968 to 1993 and, again, from 1998 to 2003. Its best electoral result was in the 1968 regional election (the first after its foundation), when the MF won 5.1% of the vote (more than 10% in the province of Udine, especially in Carnia) and three regional councillors.

Geographic entities mentioned:
surface_form: Carnia
instance_of: Valley
countries: Italy
coordinates: lat: 46.39444444
lon: 12.77416667
As District Collector of Kozhikode (Calicut), he played a pivotal role in the expansion of the Calicut airport. His efforts included revamping the Mananchira Maidan, reconstructing the building of the Kozhikode Public Library and Research Centre, and organising the 'Malabar Mahotsav' cultural festival.

Geographic entities mentioned:
surface_form: Mananchira Maidan
instance_of: Lake
countries: India
coordinates: lat: 11.254416666667
lon: 75.779972222222
Distribution and habitat. The giant coot is found from southern Peru through western Bolivia into northern Chile and northwestern Argentina. It is a bird of the Altiplano, a generally barren high elevation landscape. There it inhabits ponds and lakes, especially those with weedy shallows. It mainly occurs between but is regular as high as and occasionally wanders as far as the Pacific coast.

Geographic entities mentioned:
surface_form: Altiplano
instance_of: Plateau
countries: Bolivia
Peru
Chile
Argentina
coordinates: lat: -16.00358
lon: -69.65332
Poverty Island Light Station. The Poverty Island Light is a light house located on Poverty Island in northwestern Lake Michigan, south of Garden Peninsula. It was listed on the National Register of Historic Places in 2005 as the Poverty Island Light Station. History.

Geographic entities mentioned:
surface_form: Lake Michigan
instance_of: Lake
countries: United States
coordinates: lat: 44.007874
lon: -86.756451
Tordoki Yani. Tordoki Yani or Tardoki Yani () is the highest peak of the Sikhote-Alin Mountains. It is located in the southeast of Khabarovsk Krai to the north of the border of Primorsky Krai. It is a table mountain and rises to an elevation of 2,090 m (2077 at GSE). The mountain is the source of the river Anyuy.

Geographic entities mentioned:
surface_form: tordoki yani
instance_of: Mountain
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 48.897222222222
lon: 138.05277777778
Irrenberg. Irrenberg is a mountain of Baden-Württemberg, Germany. It is located in Zollernalbkreis.

Geographic entities mentioned:
surface_form: württemberg
instance_of: Mountain
countries: Germany
coordinates: lat: 48.7821
lon: 9.26867
surface_form: irrenberg
instance_of: Mountain
countries: Germany
coordinates: lat: 48.281111111111
lon: 8.9438888888889
Irrenberg. Irrenberg is a mountain of Baden-Württemberg, Germany. It is located in Zollernalbkreis.

Geographic entities mentioned:
surface_form: irrenberg
instance_of: Mountain
countries: Germany
coordinates: lat: 48.281111111111
lon: 8.9438888888889
By 1987, 32,000 Bukharan Jews lived in Israel, around 40% of the Bukharim. In 1990, there were riots against the Jewish population of Andijan and nearby areas. This led to most Jews in the Fergana Valley immigrating to Israel or the United States. 1990s–present. From 1989 to 2005 over 5,000 Bukharan Jews from Kyrgyzstan came to Israel due to increased hostility in the region.

Geographic entities mentioned:
surface_form: Fergana Valley
instance_of: Valley
countries: Kyrgyzstan
Uzbekistan
Tajikistan
coordinates: lat: 40.900833333333
lon: 71.757777777778
In the early 20th century, the Jewish National Fund devoted the day to planting eucalyptus trees to stop the plague of malaria in the Hula Valley; today the Fund schedules major tree-planting events in large forests every Tu BiShvat. Over a million Israelis take part in the Jewish National Fund's Tu BiShvat tree-planting activities.

Geographic entities mentioned:
surface_form: Hula Valley
instance_of: Valley
countries: Israel
coordinates: lat: 33.103333333333
lon: 35.609166666667
As a named river, it begins in Irwindale and flows southwest to its confluence in South Gate, passing through several cities (though not the city of Los Angeles). Above Irwindale, its main stem is known as Santa Anita Creek, which extends to another northwards into the San Gabriel Mountains where the source, or headwaters, of the river are found. Background.

Geographic entities mentioned:
surface_form: Santa Anita Creek
instance_of: Valley
countries: United States
coordinates: lat: 34.1717
lon: -118.032
Background. The Rio Hondo has sometimes been described as a second channel of the San Gabriel River. For much of its length, the rivers flow parallel to each other about two miles (3 km) apart. Both rivers pass through the Whittier Narrows, a natural gap in the hills which form the southern boundary of the San Gabriel Valley.

Geographic entities mentioned:
surface_form: Whittier Narrows
instance_of: Landform
countries: United States
coordinates: lat: 34.0292
lon: -118.049
surface_form: San Gabriel Valley
instance_of: Valley
countries: United States
coordinates: lat: 34.101944444444
lon: -118.10277777778
Mitaanjigamiing First Nation. &quot;Mitaanjigamiing&quot; First Nation, formerly known as Stanjikoming First Nation, is an Ojibwe First Nation band government who inhabit north of Fort Frances, Ontario, along the shores of Stanjikoming Bay of Rainy Lake. As of November, 2011, the First Nation had a total registered population of 142, of which 99 lived on their own reserve. Governance.

Geographic entities mentioned:
surface_form: Rainy Lake
instance_of: Lake
countries: Canada
United States
coordinates: lat: 48.636944444444
lon: -93.031388888889
Xaxaba Airfield. Xaxaba Airfield is an airstrip west of Xaxaba, a village in the Okavango Delta of Botswana. It serves several safari camps in the area. The runway is just outside the Moremi Game Reserve.

Geographic entities mentioned:
surface_form: Okavango Delta
instance_of: Body of water
Watercourse
countries: Botswana
coordinates: lat: -19.4
lon: 22.9
Mythimna conigera. &quot;Mythimna conigera&quot;, the brown-line bright-eye, is a moth of the family Noctuidae. Distribution. This species can be found in Europe and there is a disjunct population in the Sind Valley, Kashmir named subspecies &quot;angulifera&quot; (Moore, 1881) and east across the Palearctic from Asia Minor, Armenia, Central Asia, Siberia to Japan. Habitat.

Geographic entities mentioned:
surface_form: Sind Valley
instance_of: Valley
countries: India
coordinates: lat: 34.2892
lon: 74.8125
Personal life. Byfuglien and his wife, Emily, have three children. All of the couple's children were born in Winnipeg. Byfuglien is an avid fisherman, and competed in the 2011 Fort Frances Canadian Bass Championship on Rainy Lake. He embraced his passion for fishing after retiring from the NHL and became a pro fisher.

Geographic entities mentioned:
surface_form: Rainy Lake
instance_of: Lake
countries: Canada
United States
coordinates: lat: 48.636944444444
lon: -93.031388888889
He embraced his passion for fishing after retiring from the NHL and became a pro fisher. On August 31, 2011, Byfuglien was arrested on Lake Minnetonka and booked on suspicion of boating while intoxicated. Byfuglien pleaded guilty, and was sentenced to two days of community service on July 23, 2012.

Geographic entities mentioned:
surface_form: Lake Minnetonka
instance_of: Lake
countries: United States
coordinates: lat: 44.933333333333
lon: -93.566666666667
In John 1:29 it lacks ο Ιωαννης along with manuscripts א, A, B, K, M, N, S, U, Y, Δ, Θ, Π, Ψ, Ω, 0141, 8., 9., 565., 1192. History. Currently the manuscript is dated by the INTF to the 8th century. The codex was discovered by Gregory in 1886, who gave the first description of the codex. The codex was formerly held in the monastery of St. Andrew on Athos Peninsula. C. R.

Geographic entities mentioned:
surface_form: Athos Peninsula
instance_of: Mountain
countries: Greece
coordinates: lat: 40.15833333333333
lon: 24.327222222222222
Palgrave is located east of Orangeville, south of Alliston, west of Newmarket and north of Brampton. Geography. Palgrave is situated on the Oak Ridges Moraine, a long ridge of hilly terrain created by retreating glaciers depositing large quantities of sand and gravel sediments. The moraine is a primary source for many river systems in this part of Southern Ontario.

Geographic entities mentioned:
surface_form: Oak Ridges Moraine
instance_of: Mountain
countries: Canada
coordinates: lat: 44.05
lon: -78.86666667
The Southern Michigan League never returned to play. Battle Creen, Michigan next hosted minor league baseball when the 1919 Battle Creek Custers became members of the Class B level Michigan-Ontario League. The ballpark. The Battle Creek Crickets hosted home minor league games at Athletic Park. The ballpark was located on the northern shore of Goguac Lake near Highland Avenue & Surby Avenue.

Geographic entities mentioned:
surface_form: Goguac Lake
instance_of: Lake
countries: United States
coordinates: lat: 42.291666666667
lon: -85.208333333333
degree. While at Oxford he won the mile race in the University Sports. In the summer of 1863, with his friends Robertson and Chaytor, he ascended the Jungfrau peak in Switzerland, a notable feat at the time. On leaving university he joined the staff of Rugby School where, from 1862 to 1874, he was an Assistant Master under the headmastership of Frederick Temple.

Geographic entities mentioned:
surface_form: Jungfrau
instance_of: Mountain
countries: Switzerland
coordinates: lat: 46.536944444444
lon: 7.9625
The BCMC Trail on Grouse Mountain is so named as a legacy of the various trails established and maintained by the club on Grouse Mountain over the past century.

Geographic entities mentioned:
surface_form: Grouse Mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 49.38611111
lon: -123.07638889
The coat of arms is a shield with the image of Mount Triglav, Slovenia's highest peak, in white against a blue background at the centre; beneath it are two wavy blue lines representing the Adriatic Sea and local rivers, and above it are three six-pointed golden stars arranged in an inverted triangle which are taken from the coat of arms of the Counts of Celje, the great Slovene dynastic house of the late 14th and early 15th centuries.

Geographic entities mentioned:
surface_form: Triglav
instance_of: Mountain
countries: Slovenia
coordinates: lat: 46.378333
lon: 13.836667
This climate is possible because of the convergence of moist air of the Pacific with the Western Andes. The San Juan River runs through the area, beginning in the Farallones de Cali and flowing into the Dagua River, which is part of the greater Anchicayá River drainage. The name &quot;El Queremal&quot; comes from the local plant &quot;Cavendishia quereme&quot;.

Geographic entities mentioned:
surface_form: Farallones de Cali
instance_of: Mountain
countries: Colombia
coordinates: lat: 3.34
lon: -76.695833333333
This was the only time that the two men met; Nelson was killed at his victory at Trafalgar seven weeks later. Wellesley then served in the abortive Anglo-Russian expedition to north Germany in 1805, taking a brigade to Elbe. He then took a period of extended leave from the army and was elected as a Tory member of the British parliament for Rye in January 1806.

Geographic entities mentioned:
surface_form: Elbe
instance_of: Watercourse
countries: Czech Republic
Germany
coordinates: lat: 53.922222222222224
lon: 8.722222222222221
Red Mountain (Glacier County, Montana). Red Mountain () is located in the Lewis Range, Glacier National Park in the U.S. state of Montana. Red Mountain is north of Rising Wolf Mountain. Climate. Based on the Köppen climate classification, it is located in an alpine subarctic climate zone with long, cold, snowy winters, and cool to warm summers.

Geographic entities mentioned:
surface_form: Rising Wolf Mountain
instance_of: Mountain
countries: United States
coordinates: lat: 48.4961
lon: -113.416
surface_form: red mountain
instance_of: Mountain
countries: United States
coordinates: lat: 33.4867
lon: -86.8064
surface_form: red mountain
instance_of: Mountain
countries: United States
coordinates: lat: 47.3918
lon: -121.145
surface_form: red mountain
instance_of: Mountain
countries: United States
coordinates: lat: 48.60041
lon: -120.98678
surface_form: red mountain
instance_of: Mountain
countries: United States
coordinates: lat: 35.5231
lon: -111.876
surface_form: red mountain
instance_of: Mountain
countries: United States
coordinates: lat: 37.415277777778
lon: -121.46694444444
surface_form: red mountain
instance_of: Mountain
countries: United States
coordinates: lat: 47.45588
lon: -121.3891607
surface_form: red mountain
instance_of: Mountain
countries: United States
coordinates: lat: 45.064444444444
lon: -117.24638888889
surface_form: red mountain
instance_of: Mountain
countries: United States
coordinates: lat: 46.2979
lon: -119.441
surface_form: wolf mountain
instance_of: Mountain
countries: United States
coordinates: lat: 45.150277777778
lon: -109.91361111111
surface_form: red mountain
instance_of: Mountain
countries: United States
coordinates: lat: 42.26751
lon: -74.54952
surface_form: red mountain
instance_of: Mountain
countries: United States
coordinates: lat: 48.5356
lon: -113.424
surface_form: red mountain
instance_of: Mountain
countries: United States
coordinates: lat: 37.1122
lon: -105.181
surface_form: red mountain
instance_of: Mountain
countries: United States
coordinates: lat: 37.9036
lon: -107.702
surface_form: red mountain
instance_of: Mountain
countries: United States
coordinates: lat: 43.9783
lon: -110.872
Red Mountain (Glacier County, Montana). Red Mountain () is located in the Lewis Range, Glacier National Park in the U.S. state of Montana. Red Mountain is north of Rising Wolf Mountain. Climate. Based on the Köppen climate classification, it is located in an alpine subarctic climate zone with long, cold, snowy winters, and cool to warm summers.

Geographic entities mentioned:
surface_form: red mountain
instance_of: Mountain
countries: United States
coordinates: lat: 33.4867
lon: -86.8064
surface_form: red mountain
instance_of: Mountain
countries: United States
coordinates: lat: 47.3918
lon: -121.145
surface_form: red mountain
instance_of: Mountain
countries: United States
coordinates: lat: 48.60041
lon: -120.98678
surface_form: red mountain
instance_of: Mountain
countries: United States
coordinates: lat: 35.5231
lon: -111.876
surface_form: red mountain
instance_of: Mountain
countries: United States
coordinates: lat: 37.415277777778
lon: -121.46694444444
surface_form: red mountain
instance_of: Mountain
countries: United States
coordinates: lat: 47.45588
lon: -121.3891607
surface_form: red mountain
instance_of: Mountain
countries: United States
coordinates: lat: 45.064444444444
lon: -117.24638888889
surface_form: red mountain
instance_of: Mountain
countries: United States
coordinates: lat: 46.2979
lon: -119.441
surface_form: red mountain
instance_of: Mountain
countries: United States
coordinates: lat: 42.26751
lon: -74.54952
surface_form: red mountain (glacier county, montana)
instance_of: Mountain
countries: United States
coordinates: lat: 48.5356
lon: -113.424
surface_form: red mountain
instance_of: Mountain
countries: United States
coordinates: lat: 37.1122
lon: -105.181
surface_form: red mountain
instance_of: Mountain
countries: United States
coordinates: lat: 37.9036
lon: -107.702
surface_form: red mountain
instance_of: Mountain
countries: United States
coordinates: lat: 43.9783
lon: -110.872
Red Mountain (Glacier County, Montana). Red Mountain () is located in the Lewis Range, Glacier National Park in the U.S. state of Montana. Red Mountain is north of Rising Wolf Mountain. Climate. Based on the Köppen climate classification, it is located in an alpine subarctic climate zone with long, cold, snowy winters, and cool to warm summers.

Geographic entities mentioned:
surface_form: red mountain
instance_of: Mountain
countries: United States
coordinates: lat: 33.4867
lon: -86.8064
surface_form: red mountain
instance_of: Mountain
countries: United States
coordinates: lat: 47.3918
lon: -121.145
surface_form: red mountain
instance_of: Mountain
countries: United States
coordinates: lat: 48.60041
lon: -120.98678
surface_form: red mountain
instance_of: Mountain
countries: United States
coordinates: lat: 35.5231
lon: -111.876
surface_form: red mountain
instance_of: Mountain
countries: United States
coordinates: lat: 37.415277777778
lon: -121.46694444444
surface_form: red mountain
instance_of: Mountain
countries: United States
coordinates: lat: 47.45588
lon: -121.3891607
surface_form: red mountain
instance_of: Mountain
countries: United States
coordinates: lat: 45.064444444444
lon: -117.24638888889
surface_form: red mountain
instance_of: Mountain
countries: United States
coordinates: lat: 46.2979
lon: -119.441
surface_form: red mountain
instance_of: Mountain
countries: United States
coordinates: lat: 42.26751
lon: -74.54952
surface_form: red mountain
instance_of: Mountain
countries: United States
coordinates: lat: 48.5356
lon: -113.424
surface_form: red mountain
instance_of: Mountain
countries: United States
coordinates: lat: 37.1122
lon: -105.181
surface_form: red mountain
instance_of: Mountain
countries: United States
coordinates: lat: 37.9036
lon: -107.702
surface_form: red mountain
instance_of: Mountain
countries: United States
coordinates: lat: 43.9783
lon: -110.872
Lake Elizabeth (Fremont, California). Lake Elizabeth, located in Central Park of Fremont, California, is a man made lake with a 2 mile walkway around the lake. When at average capacity, water rises to a depth of about seven feet. About. Lake Elizabeth was named when it and the surrounding Central Park were dedicated to Fremont's sister city, Elizabeth, South Australia on March 22, 1969.

Geographic entities mentioned:
surface_form: lake elizabeth
instance_of: Lake
countries: United States
coordinates: lat: 45.064444444444
lon: -94.801666666667
surface_form: lake elizabeth
instance_of: Lake
countries: United States
coordinates: lat: 37.5486
lon: -121.962
When at average capacity, water rises to a depth of about seven feet. About. Lake Elizabeth was named when it and the surrounding Central Park were dedicated to Fremont's sister city, Elizabeth, South Australia on March 22, 1969. Central Park and Lake Elizabeth began development in 1960.

Geographic entities mentioned:
surface_form: lake elizabeth
instance_of: Lake
countries: United States
coordinates: lat: 45.064444444444
lon: -94.801666666667
surface_form: lake elizabeth
instance_of: Lake
countries: United States
coordinates: lat: 37.5486
lon: -121.962
About. Lake Elizabeth was named when it and the surrounding Central Park were dedicated to Fremont's sister city, Elizabeth, South Australia on March 22, 1969. Central Park and Lake Elizabeth began development in 1960. Central Park and the lake are visited by hundreds of people every day, and the lake is commonly used for boating and other recreational activities too.

Geographic entities mentioned:
surface_form: lake elizabeth
instance_of: Lake
countries: United States
coordinates: lat: 45.064444444444
lon: -94.801666666667
surface_form: lake elizabeth
instance_of: Lake
countries: United States
coordinates: lat: 37.5486
lon: -121.962
Many people also enjoy fishing at the lake, as it is free. Fishes that could be caught include sunfish, trout, catfish, and largemouth bass. The Aqua Adventure water park lies in Central Park on the southern shore of Lake Elizabeth. Hydrology. Lake Elizabeth has one island, named Duck Island, located in the eastern part of the lake. Mission Creek flows into Lake Elizabeth on the southern shore.

Geographic entities mentioned:
surface_form: lake elizabeth
instance_of: Lake
countries: United States
coordinates: lat: 45.064444444444
lon: -94.801666666667
surface_form: lake elizabeth
instance_of: Lake
countries: United States
coordinates: lat: 37.5486
lon: -121.962
Fishes that could be caught include sunfish, trout, catfish, and largemouth bass. The Aqua Adventure water park lies in Central Park on the southern shore of Lake Elizabeth. Hydrology. Lake Elizabeth has one island, named Duck Island, located in the eastern part of the lake. Mission Creek flows into Lake Elizabeth on the southern shore. Tunnel.

Geographic entities mentioned:
surface_form: lake elizabeth
instance_of: Lake
countries: United States
coordinates: lat: 45.064444444444
lon: -94.801666666667
surface_form: lake elizabeth
instance_of: Lake
countries: United States
coordinates: lat: 37.5486
lon: -121.962
Hydrology. Lake Elizabeth has one island, named Duck Island, located in the eastern part of the lake. Mission Creek flows into Lake Elizabeth on the southern shore. Tunnel. As part of the Warm Springs BART expansion, a cut-and-cover tunnel was built across Fremont Central Park and under Lake Elizabeth at a cost of $137 million.

Geographic entities mentioned:
surface_form: lake elizabeth
instance_of: Lake
countries: United States
coordinates: lat: 45.064444444444
lon: -94.801666666667
surface_form: lake elizabeth
instance_of: Lake
countries: United States
coordinates: lat: 37.5486
lon: -121.962
Mission Creek flows into Lake Elizabeth on the southern shore. Tunnel. As part of the Warm Springs BART expansion, a cut-and-cover tunnel was built across Fremont Central Park and under Lake Elizabeth at a cost of $137 million. Underground tracks are more expensive than surface tracks, but this lessens the impact of train operations on the park.

Geographic entities mentioned:
surface_form: lake elizabeth
instance_of: Lake
countries: United States
coordinates: lat: 45.064444444444
lon: -94.801666666667
surface_form: lake elizabeth
instance_of: Lake
countries: United States
coordinates: lat: 37.5486
lon: -121.962
Several Italian churches still retain bronze doors cast in Constantinople in the later days of the Eastern Empire, such as those presented by the members of the Pantaleone family, in the latter half of the 11th century, to the churches at Amalfi, Monte Cassino, Atrani and Monte Gargano. Similar doors are at Salerno; and St Mark's, Venice, also has doors of Greek origin. Germany.

Geographic entities mentioned:
surface_form: Monte Cassino
instance_of: Mountain
countries: Italy
coordinates: lat: 41.49
lon: 13.813888888889
Storjoen Peak. Storjoen Peak () is a salient peak 4 nautical miles (7 km) northwest of Tvora in the Sverdrup Mountains, Queen Maud Land. Plotted from air photos by the German Antarctic Expedition (1938–39).

Geographic entities mentioned:
surface_form: storjoen peak
instance_of: Mountain
coordinates: lat: -72.1167
lon: -0.2
Plotted from air photos by the German Antarctic Expedition (1938–39). Remapped by Norwegian cartographers from surveys and air photos by Norwegian-British-Swedish Antarctic Expedition (NBSAE) (1949–52) and air photos by the Norwegian expedition (1958–59) and named Storjoen (the skua).

Geographic entities mentioned:
surface_form: storjoen
instance_of: Mountain
coordinates: lat: -72.1167
lon: -0.2
The local government converted it into a museum. On the second floor is the Archivio Storico, an archive that stores and researches documents relating to the Val Bregaglia region. Additionally on the second floor there is a permanent exhibit dedicated to the history of Graubünden's pastry bakers, a tribute to Giovanni's upbringing.

Geographic entities mentioned:
surface_form: Val Bregaglia
instance_of: Valley
countries: Switzerland
coordinates: lat: 46.3324
lon: 9.514
Kirchner Peak. Kirchner Peak () is a somewhat isolated peak, high, located north-northeast of Gaylord Ridge in the Nebraska Peaks, Antarctica. It was named by the Advisory Committee on Antarctic Names after J.F. Kirchner, a member of the United States Antarctic Research Program geophysical field party during the Ross Ice Shelf Project, 1974–75 and 1976–77 seasons.

Geographic entities mentioned:
surface_form: Nebraska Peaks
instance_of: Mountain
coordinates: lat: -80.0667
lon: 159.5
surface_form: kirchner peak
instance_of: Mountain
coordinates: lat: -79.9833
lon: 159.367
Kirchner Peak. Kirchner Peak () is a somewhat isolated peak, high, located north-northeast of Gaylord Ridge in the Nebraska Peaks, Antarctica. It was named by the Advisory Committee on Antarctic Names after J.F. Kirchner, a member of the United States Antarctic Research Program geophysical field party during the Ross Ice Shelf Project, 1974–75 and 1976–77 seasons.

Geographic entities mentioned:
surface_form: field
instance_of: Mountain
coordinates: lat: -80.88333
lon: 158
Kirchner Peak. Kirchner Peak () is a somewhat isolated peak, high, located north-northeast of Gaylord Ridge in the Nebraska Peaks, Antarctica. It was named by the Advisory Committee on Antarctic Names after J.F. Kirchner, a member of the United States Antarctic Research Program geophysical field party during the Ross Ice Shelf Project, 1974–75 and 1976–77 seasons.

Geographic entities mentioned:
surface_form: kirchner peak
instance_of: Mountain
coordinates: lat: -79.9833
lon: 159.367
Mount Smithson. nkp74ctdzupbbm34ga5isknoqjhi" xml:space="preserve">#REDIRECT Mount Smithson

Geographic entities mentioned:
surface_form: mount smithson
instance_of: Mountain
coordinates: lat: -84.99916333
lon: -172.18417
surface_form: smithson
instance_of: Mountain
coordinates: lat: -84.99916333
lon: -172.18417
These deposits occur within gently dipping Late Devonian age volcanic and sedimentary rocks that are the remnants of a large epicontinental caldera complex. The regional geology in the mine area is dominated by the Mount Pleasant Caldera, the exposed part of which measures approximately 13 by 17 kilometres.

Geographic entities mentioned:
surface_form: Mount Pleasant Caldera
instance_of: Mountain
countries: Canada
coordinates: lat: 45.7378
lon: -67.3306
Mount Aka (Daisetsuzan). is a stratovolcano located in the Daisetsuzan Volcanic Group of the Ishikari Mountains, Hokkaidō, Japan.

Geographic entities mentioned:
surface_form: mount aka (daisetsuzan)
instance_of: Mountain
countries: Japan
coordinates: lat: 43.67444444
lon: 142.92666667
Geology. The Champlain Valley is the northernmost unit of a landform system known as the Great Appalachian Valley, which stretches between Quebec, Canada, to the north, and Alabama, U.S., to the south. The Champlain Valley is a physiographic section of the larger Saint Lawrence Valley, which in turn is part of the larger Appalachian physiographic division.

Geographic entities mentioned:
surface_form: Champlain Valley
instance_of: Valley
countries: United States
coordinates: lat: 44.45868
lon: -73.42617
surface_form: Great Appalachian Valley
instance_of: Valley
countries: United States
coordinates: lat: 39.5
lon: -77.83333333333333
surface_form: champlain
instance_of: Lake
countries: United States
Canada
coordinates: lat: 44.53
lon: -73.33
In this period, the Continental Army gained strength and was victorious at Saratoga. Beginning of the Revolutionary War. At the start of the Revolutionary War, British forces occupied the Champlain Valley. However, it did not take long for rebel leaders to realize the importance of controlling Lake Champlain.

Geographic entities mentioned:
surface_form: Champlain Valley
instance_of: Valley
countries: United States
coordinates: lat: 44.45868
lon: -73.42617
surface_form: champlain
instance_of: Lake
countries: United States
Canada
coordinates: lat: 44.53
lon: -73.33
Benedict Arnold shared the command with Allen, and, in early May 1775, they captured Fort Ticonderoga, Crown Point and the southern Loyalist settlement of Skenesborough. As a result of Allen's offensive attack on the Champlain Valley in 1775, the American forces controlled the Lake Champlain waterway. Siege of Quebec: 1775–1776.

Geographic entities mentioned:
surface_form: Champlain Valley
instance_of: Valley
countries: United States
coordinates: lat: 44.45868
lon: -73.42617
surface_form: champlain
instance_of: Lake
countries: United States
Canada
coordinates: lat: 44.53
lon: -73.33
surface_form: champlain
instance_of: Lake
countries: United States
Canada
coordinates: lat: 44.53
lon: -73.33
surface_form: lake champlain
instance_of: Lake
countries: United States
Canada
coordinates: lat: 44.53
lon: -73.33
Post-Revolutionary War period. Eager to take back control of Lake Champlain following the end of the Revolutionary War, Americans flocked to settle the Champlain Valley. Many individuals emigrated from Massachusetts and other New England colonies, such as Salmon Dutton, a settler of Cavendish, Vermont. Dutton emigrated in 1782 and worked as a surveyor, town official and toll-road owner.

Geographic entities mentioned:
surface_form: Champlain Valley
instance_of: Valley
countries: United States
coordinates: lat: 44.45868
lon: -73.42617
As of 2021, only one remains. Waterways. Lake Champlain has been connected to the Erie Canal via the Champlain Canal since the canal's official opening on September 9, 1823, the same day as the opening of the Erie Canal from Rochester on Lake Ontario to Albany. It connects to the St. Lawrence River via the Richelieu River, with the Chambly Canal bypassing rapids on the river since 1843.

Geographic entities mentioned:
surface_form: Lake Ontario
instance_of: Lake
countries: Canada
United States
coordinates: lat: 43.72888888888889
lon: -78.10638888888889
Chazy Reef. The Chazy Reef is an extensive Ordovician carbonate rock formation that extends from Tennessee to Quebec and Newfoundland. The oldest reefs are around &quot;The Head&quot; of the south end of Isle La Motte; slightly younger reefs are found at the Fisk Quarry, and the youngest (the famous coral reefs) are in fields to the north. History.

Geographic entities mentioned:
surface_form: rock
instance_of: Watercourse
countries: United States
Canada
coordinates: lat: 44.9889
lon: -73.0882
Lake Champlain. Lake Champlain (;,) is a large natural freshwater lake in North America. With a length of and surface area over, it lies mostly between the U.S. states of New York and Vermont, but also extends north into the Canadian province of Quebec.

Geographic entities mentioned:
surface_form: champlain
instance_of: Lake
countries: United States
Canada
coordinates: lat: 44.53
lon: -73.33
surface_form: lake champlain
instance_of: Lake
countries: United States
Canada
coordinates: lat: 44.53
lon: -73.33
There are a number of islands in the lake; the largest include Grand Isle, Isle La Motte and North Hero: all part of Grand Isle County, Vermont. Because of Lake Champlain's connections both to the St. Lawrence Seaway via the Richelieu River, and to the Hudson River via the Champlain Canal, Lake Champlain is sometimes referred to as &quot;The Sixth Great Lake&quot;.

Geographic entities mentioned:
surface_form: champlain
instance_of: Lake
countries: United States
Canada
coordinates: lat: 44.53
lon: -73.33
surface_form: champlain
instance_of: Lake
countries: United States
Canada
coordinates: lat: 44.53
lon: -73.33
surface_form: champlain
instance_of: Lake
countries: United States
Canada
coordinates: lat: 44.53
lon: -73.33
surface_form: lake champlain
instance_of: Lake
countries: United States
Canada
coordinates: lat: 44.53
lon: -73.33
surface_form: lake champlain
instance_of: Lake
countries: United States
Canada
coordinates: lat: 44.53
lon: -73.33
Geology. The Champlain Valley is the northernmost unit of a landform system known as the Great Appalachian Valley, which stretches between Quebec, Canada, to the north, and Alabama, U.S., to the south. The Champlain Valley is a physiographic section of the larger Saint Lawrence Valley, which in turn is part of the larger Appalachian physiographic division.

Geographic entities mentioned:
surface_form: champlain
instance_of: Lake
countries: United States
Canada
coordinates: lat: 44.53
lon: -73.33
Hydrology. Lake Champlain covers approximately, making it the thirteenth-largest lake by area in the U.S. It lies at an elevation of, is, has a shoreline, averages in width, has an average depth of, a maximum depth of, and holds some of water.

Geographic entities mentioned:
surface_form: champlain
instance_of: Lake
countries: United States
Canada
coordinates: lat: 44.53
lon: -73.33
surface_form: lake champlain
instance_of: Lake
countries: United States
Canada
coordinates: lat: 44.53
lon: -73.33
It lies at an elevation of, is, has a shoreline, averages in width, has an average depth of, a maximum depth of, and holds some of water. Lake Champlain is in the Champlain Valley between the Green Mountains of Vermont and the Adirondack Mountains of New York, drained northward by the Richelieu River into the St. Lawrence River at Sorel-Tracy, Quebec, northeast and downstream of Montreal.

Geographic entities mentioned:
surface_form: champlain
instance_of: Lake
countries: United States
Canada
coordinates: lat: 44.53
lon: -73.33
surface_form: champlain
instance_of: Lake
countries: United States
Canada
coordinates: lat: 44.53
lon: -73.33
In New York, it is fed by the Ausable, Boquet, Great Chazy, La Chute, Little Ausable, Little Chazy, Salmon and Saranac rivers, along with Putnam Creek. In Quebec, it is fed by the Pike River. It is connected to the Hudson River by the Champlain Canal. Parts of the lake freeze each winter, and in some winters the entire lake surface freezes, referred to as &quot;closing&quot;.

Geographic entities mentioned:
surface_form: champlain
instance_of: Lake
countries: United States
Canada
coordinates: lat: 44.53
lon: -73.33
Colonial America and the Revolutionary War. New France allocated concessions all along Lake Champlain to French settlers and built forts to defend the waterways. In colonial times, Lake Champlain was used as a water (or, in winter, ice) passage between the Saint Lawrence and Hudson valleys.

Geographic entities mentioned:
surface_form: champlain
instance_of: Lake
countries: United States
Canada
coordinates: lat: 44.53
lon: -73.33
surface_form: lake champlain
instance_of: Lake
countries: United States
Canada
coordinates: lat: 44.53
lon: -73.33
The necessity of controlling the two forts at Ticonderoga and Crown Point placed Lake Champlain as a strategic arena during the Revolutionary War. By taking control of these forts, Americans not only gained heavy artillery, but control of a vast water highway as well: Lake Champlain provided a direct invasion route to British Canada.

Geographic entities mentioned:
surface_form: champlain
instance_of: Lake
countries: United States
Canada
coordinates: lat: 44.53
lon: -73.33
surface_form: lake champlain
instance_of: Lake
countries: United States
Canada
coordinates: lat: 44.53
lon: -73.33
Immediately after taking Forts Ticonderoga and Crown Point, the Americans began planning an attack on British Canada. The American siege of Quebec was a two-pronged assault and occurred throughout the winter of 1775–1776. Brigadier General Richard Montgomery led the first assault up the Champlain Valley into Canada, while Benedict Arnold led a second army to Quebec via the Maine wilderness.

Geographic entities mentioned:
surface_form: champlain
instance_of: Lake
countries: United States
Canada
coordinates: lat: 44.53
lon: -73.33
The reinforcements traveled hundreds of miles up the frozen Lake Champlain and St. Lawrence River, but were too late and too few to influence a successful siege of Quebec. In May 1776, with the arrival of a British convoy carrying 10,000 British and Hessian troops to Canada, the Continental forces retreated back down the Champlain Valley to reevaluate their strategy.

Geographic entities mentioned:
surface_form: champlain
instance_of: Lake
countries: United States
Canada
coordinates: lat: 44.53
lon: -73.33
Both British and American forces spent the summer of 1776 building their naval fleets, at opposite ends of Lake Champlain. By the October 1776, the Continental Army had 16 operating naval vessels on Lake Champlain: a great increase to the four small ships they had at the beginning of the summer.

Geographic entities mentioned:
surface_form: champlain
instance_of: Lake
countries: United States
Canada
coordinates: lat: 44.53
lon: -73.33
surface_form: lake champlain
instance_of: Lake
countries: United States
Canada
coordinates: lat: 44.53
lon: -73.33
General Benedict Arnold commanded the American naval fleet on Lake Champlain, which was composed of volunteers and soldiers drafted from the Northern Army. With great contrast to the Continental navy, experienced Royal Navy officers, British seamen and Hessian artillerymen manned the British fleet on Lake Champlain.

Geographic entities mentioned:
surface_form: champlain
instance_of: Lake
countries: United States
Canada
coordinates: lat: 44.53
lon: -73.33
surface_form: lake champlain
instance_of: Lake
countries: United States
Canada
coordinates: lat: 44.53
lon: -73.33
With great contrast to the Continental navy, experienced Royal Navy officers, British seamen and Hessian artillerymen manned the British fleet on Lake Champlain. By the end of the summer of 1776, the opposing armies were prepared to battle over the strategic advantage of controlling Lake Champlain. Battle of Valcour Island.

Geographic entities mentioned:
surface_form: champlain
instance_of: Lake
countries: United States
Canada
coordinates: lat: 44.53
lon: -73.33
surface_form: lake champlain
instance_of: Lake
countries: United States
Canada
coordinates: lat: 44.53
lon: -73.33
With no hope of fighting off the powerful British navy, Arnold ordered his men to run their five vessels aground in Ferris Bay, Panton, Vermont. The depleted Continental army escaped on land back to Fort Ticonderoga and Mount Independence; however, they no longer controlled the Lake Champlain waterway.

Geographic entities mentioned:
surface_form: champlain
instance_of: Lake
countries: United States
Canada
coordinates: lat: 44.53
lon: -73.33
surface_form: champlain
instance_of: Lake
countries: United States
Canada
coordinates: lat: 44.53
lon: -73.33
surface_form: lake champlain
instance_of: Lake
countries: United States
Canada
coordinates: lat: 44.53
lon: -73.33
surface_form: lake champlain
instance_of: Lake
countries: United States
Canada
coordinates: lat: 44.53
lon: -73.33
The depleted Continental army escaped on land back to Fort Ticonderoga and Mount Independence; however, they no longer controlled the Lake Champlain waterway. The approaching winter of 1776–1777 restricted British movement along the recently controlled Lake Champlain.

Geographic entities mentioned:
surface_form: champlain
instance_of: Lake
countries: United States
Canada
coordinates: lat: 44.53
lon: -73.33