Sarmila/GeoWiki-Features huggingface dataset:
The fault reappears at surface east of Tamalameque, Cesar, where it continues south-southeastward into the Eastern Ranges in the departments of Norte de Santander and Santander. The fault can be traced until San Andrés, Santander. The Bucaramanga Fault possibly continues as the compressional Boyacá and Soapaga Faults on the Altiplano Cundiboyacense. Tectonic setting.

Geographic entities mentioned:
surface_form: Altiplano Cundiboyacense
instance_of: Plateau
countries: Colombia
coordinates: lat: 5.532209
lon: -73.362877
Long Valley (Kane County, Utah). The Long Valley of Utah is a long valley located in western Kane County. The valley is located in source water regions of waters flowing north, south, and southwest, in the west of the &quot;High Plateaus section&quot; of the Colorado Plateau; the High Plateaus section also extends into northern Arizona, the region north of the Grand Canyon.

Geographic entities mentioned:
surface_form: Colorado Plateau
instance_of: Plateau
countries: United States
coordinates: lat: 37
lon: -110
surface_form: grand canyon
instance_of: Valley
countries: United States
coordinates: lat: 38.65888889
lon: -91.10388889
surface_form: colorado plateau
instance_of: Plateau
countries: United States
coordinates: lat: 37
lon: -110
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 34.155833333333334
lon: -118.28777777777778
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 61.3833
lon: -150.25
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 47.7174
lon: -117.047423
Long Valley is on the east border of Kolob Terrace; the forested Markagunt and Paunsaugunt Plateaus border northwest, and northeast. East is a mountain region water divide, and the south-flowing Kanab Creek in its narrow river valley, (a north tributary to the Colorado River). The northern half of Long Valley and the two plateaus lie in the Dixie National Forest.

Geographic entities mentioned:
surface_form: Markagunt
instance_of: Plateau
countries: United States
coordinates: lat: 37.6167
lon: -112.833
surface_form: Paunsaugunt Plateau
instance_of: Plateau
countries: United States
coordinates: lat: 37.5
lon: -112.38444444444
Description. Long Valley is mostly a rivercourse valley of the East Fork Virgin River. The north contains a parallel valley in the northwest, which collects long streams flowing southeasterly off the water divide at the south-southeast of the Markagunt Plateau; the other side of the divide contains northeast-flowing Swains Creek. 3 river sources.

Geographic entities mentioned:
surface_form: Markagunt Plateau
instance_of: Plateau
countries: United States
coordinates: lat: 37.6167
lon: -112.833
surface_form: markagunt plateau
instance_of: Plateau
countries: United States
coordinates: lat: 37.6167
lon: -112.833
The source of Kanab Creek is on the southwest of the Paunsaugunt Plateau; at the source region, east, Upper Kanab Creek flows northeast, as a southwest tributary to the north-flowing &quot;East Sevier River&quot;. West of the Kanab Creek source is the source of East Fork Virgin River, in the region at Long Valley Junction. The junction lies just northwest of Alton, and the Alton Amphitheater.

Geographic entities mentioned:
surface_form: Paunsaugunt Plateau
instance_of: Plateau
countries: United States
coordinates: lat: 37.5
lon: -112.38444444444
surface_form: paunsaugunt plateau
instance_of: Plateau
countries: United States
coordinates: lat: 37.5
lon: -112.38444444444
The south end of the Stout Canyon Road connects to Long Valley's center region, US&8209;89, just west of Spencer Bench. Another route exits west and northwest off Stout Canyon Road; it connects to Swains Creek Road, a northeast-flowing stream, at the northeast of Kolob Terrace, and on the south perimeter of the Markagunt Plateau.

Geographic entities mentioned:
surface_form: Markagunt Plateau
instance_of: Plateau
countries: United States
coordinates: lat: 37.6167
lon: -112.833
surface_form: markagunt plateau
instance_of: Plateau
countries: United States
coordinates: lat: 37.6167
lon: -112.833
3 river sources. The east perimeter of Long Valley is a minor mountain peak section and water divide; east of the divide is the Alton Amphitheater, and Kanab Creek flows southerly to meet the Colorado River, in the Grand Canyon.

Geographic entities mentioned:
surface_form: grand canyon
instance_of: Valley
countries: United States
coordinates: lat: 38.65888889
lon: -91.10388889
surface_form: long valley
instance_of: Landform
countries: United States
coordinates: lat: 37.716666666667
lon: -118.88416666667
surface_form: long valley
instance_of: Valley
countries: United States
coordinates: lat: 39.6833
lon: -115.722
surface_form: long valley
instance_of: Valley
countries: United States
coordinates: lat: 37.3789
lon: -112.573
Long Valley (Kane County, Utah). The Long Valley of Utah is a long valley located in western Kane County. The valley is located in source water regions of waters flowing north, south, and southwest, in the west of the &quot;High Plateaus section&quot; of the Colorado Plateau; the High Plateaus section also extends into northern Arizona, the region north of the Grand Canyon.

Geographic entities mentioned:
surface_form: long valley
instance_of: Landform
countries: United States
coordinates: lat: 37.716666666667
lon: -118.88416666667
surface_form: long valley
instance_of: Valley
countries: United States
coordinates: lat: 39.6833
lon: -115.722
surface_form: long valley (kane county, utah)
instance_of: Valley
countries: United States
coordinates: lat: 37.3789
lon: -112.573
Long Valley (Kane County, Utah). The Long Valley of Utah is a long valley located in western Kane County. The valley is located in source water regions of waters flowing north, south, and southwest, in the west of the &quot;High Plateaus section&quot; of the Colorado Plateau; the High Plateaus section also extends into northern Arizona, the region north of the Grand Canyon.

Geographic entities mentioned:
surface_form: long valley
instance_of: Landform
countries: United States
coordinates: lat: 37.716666666667
lon: -118.88416666667
surface_form: long valley
instance_of: Landform
countries: United States
coordinates: lat: 37.716666666667
lon: -118.88416666667
surface_form: long valley
instance_of: Valley
countries: United States
coordinates: lat: 39.6833
lon: -115.722
surface_form: long valley
instance_of: Valley
countries: United States
coordinates: lat: 39.6833
lon: -115.722
surface_form: long valley
instance_of: Valley
countries: United States
coordinates: lat: 37.3789
lon: -112.573
surface_form: long valley
instance_of: Valley
countries: United States
coordinates: lat: 37.3789
lon: -112.573
East is a mountain region water divide, and the south-flowing Kanab Creek in its narrow river valley, (a north tributary to the Colorado River). The northern half of Long Valley and the two plateaus lie in the Dixie National Forest. Glendale, Utah is located at the south end of the valley, on the East Fork Virgin River. U.S.

Geographic entities mentioned:
surface_form: long valley
instance_of: Landform
countries: United States
coordinates: lat: 37.716666666667
lon: -118.88416666667
surface_form: long valley
instance_of: Valley
countries: United States
coordinates: lat: 39.6833
lon: -115.722
surface_form: long valley
instance_of: Valley
countries: United States
coordinates: lat: 37.3789
lon: -112.573
East is a mountain region water divide, and the south-flowing Kanab Creek in its narrow river valley, (a north tributary to the Colorado River). The northern half of Long Valley and the two plateaus lie in the Dixie National Forest. Glendale, Utah is located at the south end of the valley, on the East Fork Virgin River. U.S.

Geographic entities mentioned:
surface_form: long valley
instance_of: Landform
countries: United States
coordinates: lat: 37.716666666667
lon: -118.88416666667
surface_form: long valley
instance_of: Landform
countries: United States
coordinates: lat: 37.716666666667
lon: -118.88416666667
surface_form: long valley
instance_of: Valley
countries: United States
coordinates: lat: 39.6833
lon: -115.722
surface_form: long valley
instance_of: Valley
countries: United States
coordinates: lat: 39.6833
lon: -115.722
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 34.155833333333334
lon: -118.28777777777778
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 34.155833333333334
lon: -118.28777777777778
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 61.3833
lon: -150.25
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 61.3833
lon: -150.25
surface_form: long valley
instance_of: Valley
countries: United States
coordinates: lat: 37.3789
lon: -112.573
surface_form: long valley
instance_of: Valley
countries: United States
coordinates: lat: 37.3789
lon: -112.573
surface_form: river valley
instance_of: Valley
countries: United States
coordinates: lat: 35.36
lon: -93.37
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 47.7174
lon: -117.047423
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 47.7174
lon: -117.047423
The East Fork Virgin River flows due-south, from near the valley center, then just south of Glendale, the river starts its southwesterly course. The sourcewaters are in the valley's northeast terminus region in the Long Valley Junction area. Description. Long Valley is mostly a rivercourse valley of the East Fork Virgin River.

Geographic entities mentioned:
surface_form: long valley
instance_of: Landform
countries: United States
coordinates: lat: 37.716666666667
lon: -118.88416666667
surface_form: long valley
instance_of: Valley
countries: United States
coordinates: lat: 39.6833
lon: -115.722
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 34.155833333333334
lon: -118.28777777777778
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 61.3833
lon: -150.25
surface_form: long valley
instance_of: Valley
countries: United States
coordinates: lat: 37.3789
lon: -112.573
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 47.7174
lon: -117.047423
The source of Kanab Creek is on the southwest of the Paunsaugunt Plateau; at the source region, east, Upper Kanab Creek flows northeast, as a southwest tributary to the north-flowing &quot;East Sevier River&quot;. West of the Kanab Creek source is the source of East Fork Virgin River, in the region at Long Valley Junction. The junction lies just northwest of Alton, and the Alton Amphitheater.

Geographic entities mentioned:
surface_form: long valley
instance_of: Landform
countries: United States
coordinates: lat: 37.716666666667
lon: -118.88416666667
surface_form: long valley
instance_of: Valley
countries: United States
coordinates: lat: 39.6833
lon: -115.722
surface_form: long valley
instance_of: Valley
countries: United States
coordinates: lat: 37.3789
lon: -112.573
West of the Kanab Creek source is the source of East Fork Virgin River, in the region at Long Valley Junction. The junction lies just northwest of Alton, and the Alton Amphitheater. The East Fork Virgin River flows south through Long Valley, then southwest to meet the Virgin River, which is a northeast tributary to Lake Mead. Access, and valley routes.

Geographic entities mentioned:
surface_form: long valley
instance_of: Landform
countries: United States
coordinates: lat: 37.716666666667
lon: -118.88416666667
surface_form: long valley
instance_of: Valley
countries: United States
coordinates: lat: 39.6833
lon: -115.722
surface_form: long valley
instance_of: Valley
countries: United States
coordinates: lat: 37.3789
lon: -112.573
US&8209;89 is the major access to the valley, from Mount Carmel-Orderville, southwest of Glendale. Another paved route enters the valley, and Glendale from the east, (&quot;Lower Kanab Creek to Alton Rd&quot;); the route is from US&8209;89, east of Kanab, and traverses north, then northeast to Long Valley, after going through west perimeter areas of the Grand Staircase–Escalante National Monument.

Geographic entities mentioned:
surface_form: long valley
instance_of: Landform
countries: United States
coordinates: lat: 37.716666666667
lon: -118.88416666667
surface_form: long valley
instance_of: Landform
countries: United States
coordinates: lat: 37.716666666667
lon: -118.88416666667
surface_form: long valley
instance_of: Valley
countries: United States
coordinates: lat: 39.6833
lon: -115.722
surface_form: long valley
instance_of: Valley
countries: United States
coordinates: lat: 39.6833
lon: -115.722
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 34.155833333333334
lon: -118.28777777777778
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 61.3833
lon: -150.25
surface_form: long valley
instance_of: Valley
countries: United States
coordinates: lat: 37.3789
lon: -112.573
surface_form: long valley
instance_of: Valley
countries: United States
coordinates: lat: 37.3789
lon: -112.573
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 47.7174
lon: -117.047423
The Alton Amphitheater is at a section of the Pink Cliffs, and the source region of south-flowing (to the Colorado River), Kanab Creek, which lies adjacent to the north-northeast. The northwest of the valley contains Stout Canyon Road, through Stout Canyon, a paved route to Utah State Route 14 on the water divide, (Great Basin Divide), west of Long Valley Junction.

Geographic entities mentioned:
surface_form: long valley
instance_of: Landform
countries: United States
coordinates: lat: 37.716666666667
lon: -118.88416666667
surface_form: long valley
instance_of: Valley
countries: United States
coordinates: lat: 39.6833
lon: -115.722
surface_form: long valley
instance_of: Valley
countries: United States
coordinates: lat: 37.3789
lon: -112.573
The northwest of the valley contains Stout Canyon Road, through Stout Canyon, a paved route to Utah State Route 14 on the water divide, (Great Basin Divide), west of Long Valley Junction. The south end of the Stout Canyon Road connects to Long Valley's center region, US&8209;89, just west of Spencer Bench.

Geographic entities mentioned:
surface_form: long valley
instance_of: Landform
countries: United States
coordinates: lat: 37.716666666667
lon: -118.88416666667
surface_form: long valley
instance_of: Valley
countries: United States
coordinates: lat: 39.6833
lon: -115.722
surface_form: long valley
instance_of: Valley
countries: United States
coordinates: lat: 37.3789
lon: -112.573
The junction lies just northwest of Alton, and the Alton Amphitheater. The East Fork Virgin River flows south through Long Valley, then southwest to meet the Virgin River, which is a northeast tributary to Lake Mead. Access, and valley routes. US&8209;89 is the major access to the valley, from Mount Carmel-Orderville, southwest of Glendale.

Geographic entities mentioned:
surface_form: mount carmel
instance_of: Mountain
countries: United States
coordinates: lat: 41.430636
lon: -72.890767
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 34.155833333333334
lon: -118.28777777777778
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 61.3833
lon: -150.25
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 47.7174
lon: -117.047423
East is a mountain region water divide, and the south-flowing Kanab Creek in its narrow river valley, (a north tributary to the Colorado River). The northern half of Long Valley and the two plateaus lie in the Dixie National Forest. Glendale, Utah is located at the south end of the valley, on the East Fork Virgin River. U.S.

Geographic entities mentioned:
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 34.155833333333334
lon: -118.28777777777778
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 61.3833
lon: -150.25
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 47.7174
lon: -117.047423
The East Fork Virgin River flows due-south, from near the valley center, then just south of Glendale, the river starts its southwesterly course. The sourcewaters are in the valley's northeast terminus region in the Long Valley Junction area. Description. Long Valley is mostly a rivercourse valley of the East Fork Virgin River.

Geographic entities mentioned:
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 34.155833333333334
lon: -118.28777777777778
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 61.3833
lon: -150.25
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 47.7174
lon: -117.047423
Long Valley is on the east border of Kolob Terrace; the forested Markagunt and Paunsaugunt Plateaus border northwest, and northeast. East is a mountain region water divide, and the south-flowing Kanab Creek in its narrow river valley, (a north tributary to the Colorado River). The northern half of Long Valley and the two plateaus lie in the Dixie National Forest.

Geographic entities mentioned:
surface_form: river valley
instance_of: Valley
countries: United States
coordinates: lat: 35.36
lon: -93.37
KCB Group. KCB Group Limited, also known as the KCB Group, is a financial services holding company based in the African Great Lakes region. The Group's headquarters are in Nairobi, Kenya, with its subsidiaries being KCB Bank Kenya Limited, KCB Bank Burundi Limited, KCB Bank Rwanda Limited, KCB Bank South Sudan Limited, KCB Bank Tanzania Limited, KCB TMB Congo and KCB Bank Uganda Limited. Overview.

Geographic entities mentioned:
surface_form: African Great Lakes
instance_of: Group of lakes
countries: Burundi
Zambia
Kenya
Democratic Republic of the Congo
Malawi
Mozambique
Rwanda
Tanzania
Uganda
Ethiopia
coordinates: lat: -8
lon: 35
San José, Petén. San José is a municipality in the Petén Department of Guatemala. It contains 3,602 people. It lies on the north shore of Lake Petén Itzá and is located a few kilometers from the Classic Period Maya ruin of Motul de San José. El Zotz is also located in the municipality. Sports.

Geographic entities mentioned:
surface_form: Lake Petén Itzá
instance_of: Lake
countries: Guatemala
coordinates: lat: 16.983333333333
lon: -89.8
The FGC fund-raise money and work to create awareness of the watershed and its importance to the area. The creek passes through Hilltop Green, under Interstate 80 via pipes, down a small canyon alongside Hilltop Plaza Shopping Center, and then through culverts to a gorge where it has been dammed to create Hilltop Lake.

Geographic entities mentioned:
surface_form: Hilltop Lake
instance_of: Lake
countries: United States
coordinates: lat: 37.986
lon: -122.328
History. The Hoendiep originally ran from a point west of the Groninger &quot;Aapoort&quot; to De Poffert. From there, to get to Friesland, sailors sailed via the (now largely disappeared) to the. They followed this canal to Briltil and from there went via the Niekerksterdiep and the to the Burgumer Mar. The extension of the Hoendiep between Briltil and the is called the &quot;Stille Diep&quot;.

Geographic entities mentioned:
surface_form: Burgumer Mar
instance_of: Lake
countries: Netherlands
coordinates: lat: 53.189722
lon: 6.041944
Bathyclarias worthingtoni. &quot;Bathyclarias worthingtoni&quot; is a species of airbreathing catfish endemic to Lake Malawi, in the countries of Malawi, Mozambique and Tanzania. This species grows to a length of SL. This species is commercially caught for human consumption.

Geographic entities mentioned:
surface_form: Lake Malawi
instance_of: Lake
countries: Malawi
Mozambique
Tanzania
coordinates: lat: -12.183333333333
lon: 34.366666666667
In the late 19th century, thought that the Yakuts had their origin somewhere to the south of the Lena River, an idea which informed contemporary attempts at explanation of the origin of the Olonkhos. In 1927 P.A. Oyunsky inferred that the Yakuts originated in the Aral Sea area, moving via the Transbaikal to the Lena River basin, using the Olonkhos as a source themselves. Ethnographer G.V.

Geographic entities mentioned:
surface_form: Aral Sea
instance_of: Lake
countries: Kazakhstan
Uzbekistan
Russian Empire
Soviet Union
coordinates: lat: 45
lon: 60
He linked their origins to the western Baikal region, where the Orkhon-Yenisei script using Guligans and Qurykans lived, and suggested that those tribes ancestors were the Yakut's ancestors - so-called &quot;forest peoples&quot;, who lived east of the Yenisei Kyrgyz in lowlands around the Selenga River, on the banks of Lake Baikal, and around the Angara River. In the 1970s G.U.

Geographic entities mentioned:
surface_form: Lake Baikal
instance_of: Lake
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 53.30277778
lon: 108.00472222
The causeway passes over marshland adjacent to the southern end of Chincoteague Bay and includes bridges over Mosquito Creek, Cockle Creek, Queen Sound Channel, and Wire Narrows. A fifth bridge curves to the north and then east around the northern end of Marsh Island to cross Black Narrows and Chincoteague Channel onto Chincoteague Island.

Geographic entities mentioned:
surface_form: Chincoteague Channel
instance_of: Landform
countries: United States
coordinates: lat: 37.91611111
lon: -75.39916667
Paniai Regency. Paniai Regency is one of the regencies (&quot;kabupaten&quot;) in Central Papua Province of Indonesia. It is named after the Paniai Lakes. It covers an area of 6,525.25 km2, and had a population of 153,432 at the 2010 Census and 220,410 at the 2020 Census; the official estimate as of mid-2024 was 227,254 - comprising 124,260 males and 102,994 females.

Geographic entities mentioned:
surface_form: Paniai Lakes
instance_of: Group of lakes
countries: Indonesia
coordinates: lat: -3.9022222222222
lon: 136.31777777778
Alabama Hills. The Alabama Hills are a range of hills and rock formations near the eastern slope of the Sierra Nevada in the Owens Valley, west of Lone Pine in Inyo County, California. Though geographically separate from the Sierra Nevada, they are part of the same geological formation. Alabama Hills National Scenic Area. Beginning on May 24, 1969, the Alabama Hills were managed by the U.S.

Geographic entities mentioned:
surface_form: Owens Valley
instance_of: Valley
countries: United States
coordinates: lat: 36.8025
lon: -118.199722
Alabama Hills National Scenic Area. Beginning on May 24, 1969, the Alabama Hills were managed by the U.S. Bureau of Land Management (BLM) as the Alabama Hills Recreation Area. In March 2019, the U.S. Congress redesignated the area as the Alabama Hills National Scenic Area. Camping. The Alabama Hills serve as a gateway to Mount Whitney and the Eastern Sierra Nevada.

Geographic entities mentioned:
surface_form: Mount Whitney
instance_of: Mountain
countries: United States
coordinates: lat: 36.57861111111111
lon: -118.29194444444444
The difference in shape and color can be accounted for by a difference in weathering. Mount Whitney, the tallest mountain in the contiguous United States, towers nine thousand feet above this low range, which itself is above the floor of Owens Valley. Gravity surveys indicate that the Owens Valley is filled with about of sediment and that the hills are the tip of a very steep escarpment.

Geographic entities mentioned:
surface_form: Mount Whitney
instance_of: Mountain
countries: United States
coordinates: lat: 36.57861111111111
lon: -118.29194444444444
surface_form: Owens Valley
instance_of: Valley
countries: United States
coordinates: lat: 36.8025
lon: -118.199722
When the &quot;Alabama&quot; was finally sunk off the coast of Normandy by the USS &quot;Kearsarge&quot; in 1864, prospectors sympathetic to the Union named a mining district, a mountain pass, a mountain peak, and a town after the &quot;Kearsarge&quot;. Filming location.

Geographic entities mentioned:
surface_form: mountain peak
instance_of: Mountain
countries: United States
coordinates: lat: 36.7891
lon: -118.34732
Wila Sirka (Potosí). Wila Sirka (Aymara &quot;wila&quot; blood, red, &quot;sirka&quot; vein of the body or a mine, &quot;red vein&quot;, also spelled &quot;Wila Sirca&quot;) is a mountain in the Bolivian Andes. It is located in the Potosí Department, Tomás Frías Province, Yocalla Municipality.

Geographic entities mentioned:
surface_form: wila sirka
instance_of: Mountain
countries: Bolivia
coordinates: lat: -18.9647
lon: -66.6825
surface_form: wila sirka (potosí)
instance_of: Mountain
countries: Bolivia
coordinates: lat: -19.47222222
lon: -65.99777778
Wila Sirka (Potosí). Wila Sirka (Aymara &quot;wila&quot; blood, red, &quot;sirka&quot; vein of the body or a mine, &quot;red vein&quot;, also spelled &quot;Wila Sirca&quot;) is a mountain in the Bolivian Andes. It is located in the Potosí Department, Tomás Frías Province, Yocalla Municipality.

Geographic entities mentioned:
surface_form: wila sirka
instance_of: Mountain
countries: Bolivia
coordinates: lat: -18.9647
lon: -66.6825
surface_form: wila sirka
instance_of: Mountain
countries: Bolivia
coordinates: lat: -19.47222222
lon: -65.99777778
Major attractions include the capital Augsburg; several other old cities including Donauwörth, Nördlingen, Memmingen, Mindelheim, Kaufbeuren and Kempten; the Ottobeuren Abbey and the scenic attractions of the River Danube in the north; the Allgäu in the south; the Allgäu Alps with mount Hochfrottspitze, mount Hochvogel and Oberstdorf; and the royal castles of Hohenschwangau, Neuschwanstein and Füssen.

Geographic entities mentioned:
surface_form: Hochfrottspitze
instance_of: Mountain
countries: Germany
Austria
coordinates: lat: 47.29611111111111
lon: 10.293055555555556
surface_form: Hochvogel
instance_of: Mountain
countries: Germany
Austria
coordinates: lat: 47.3803625
lon: 10.4367656
Takaotozan Railway. 70s32c0xflrun78y568y9s7vv0lsc" xml:space="preserve">The is a transport company in Hachiōji, Tokyo, Japan. The company operates a funicular line and a ropeway to Mount Takao, a popular destination for mountain trekking among Tokyo residents. The company was founded on September 29, 1921. Funicular==.

Geographic entities mentioned:
surface_form: Mount Takao
instance_of: Mountain
countries: Japan
coordinates: lat: 35.625277777778
lon: 139.24361111111
The historic town centre is well preserved and is protected as an urban monument reservation. Etymology. Although the town's Czech name translates directly to 'camp' or 'encampment', these words were derived from the Tábor's name, and the town was named after the biblical Mount Tabor located in Israel. The town also gave its name to the Taborites, a radical wing of the Hussites.

Geographic entities mentioned:
surface_form: Mount Tabor
instance_of: Mountain
countries: Israel
coordinates: lat: 32.68625
lon: 35.392916666667
San Joaquin Valley League. The San Joaquin Valley League was a minor league baseball league that operated from 1910 through 1911. The league operated primarily in the San Joaquin Valley in California. The league disbanded on July 18, 1911. The Bakersfield Drillers and Tulare Merchants won league championships. 1910 San Joaquin Valley League. Tulare disbanded August 8; Coalinga disbanded August 18.

Geographic entities mentioned:
surface_form: San Joaquin Valley
instance_of: Valley
countries: United States
coordinates: lat: 36.628888888889
lon: -120.185
Pressmen's Home, Tennessee. Pressmen's Home is a non-abandoned ghost town and former headquarters for the International Printing Pressmen and Assistants' Union of North America from 1911 to 1967, in the Poor Valley area of Hawkins County, Tennessee, United States, nine miles north of Rogersville.

Geographic entities mentioned:
surface_form: Poor Valley
instance_of: Valley
countries: United States
coordinates: lat: 36.185555555556
lon: -83.695555555556
Tourism. The Strömsholm Canal has been restored and is a popular route for small yachts. One can navigate from Strömsholm Palace, one of the Royal Palaces in Sweden at lake Mälaren to Fagersta and Smedjebacken through several canal locks and lakes, a total distance of 100 km. Ecomuseum Bergslagen gives an in-depth view of how the early industrialization evolved in the Bergslagen region.

Geographic entities mentioned:
surface_form: Mälaren
instance_of: Lake
countries: Sweden
coordinates: lat: 59.5
lon: 17.2
Mount Oso. Mount Oso () is a mountain in Western Stanislaus County, California, and is located on the Diablo Range. At feet in elevation, it is the third highest point in Stanislaus County. There are many radio stations and an unused forest fire lookout tower on the mountain. It appears in the City of Modesto's logo due to its predominance in the area's skyline. History.

Geographic entities mentioned:
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instance_of: Mountain
countries: United States
coordinates: lat: 32.2925
lon: -106.69777777778
surface_form: mount oso
instance_of: Mountain
countries: United States
coordinates: lat: 37.5074
lon: -121.374
surface_form: mount oso
instance_of: Mountain
countries: United States
coordinates: lat: 37.6072
lon: -107.494
It appears in the City of Modesto's logo due to its predominance in the area's skyline. History. Mount Oso, (&quot;oso&quot; - Spanish for bear), was probably discovered by
Gabriel Moraga during his expeditions in the Central Valley. This mountain can clearly
be seen in Modesto, California, and has a beautiful contrast with the almond orchards.

Geographic entities mentioned:
surface_form: central valley
instance_of: Valley
countries: United States
coordinates: lat: 37.706111111111
lon: -120.99138888889
surface_form: mount oso
instance_of: Mountain
countries: United States
coordinates: lat: 37.5074
lon: -121.374
surface_form: mount oso
instance_of: Mountain
countries: United States
coordinates: lat: 37.6072
lon: -107.494
Mount Oso. Mount Oso () is a mountain in Western Stanislaus County, California, and is located on the Diablo Range. At feet in elevation, it is the third highest point in Stanislaus County. There are many radio stations and an unused forest fire lookout tower on the mountain. It appears in the City of Modesto's logo due to its predominance in the area's skyline. History.

Geographic entities mentioned:
surface_form: mount oso
instance_of: Mountain
countries: United States
coordinates: lat: 37.5074
lon: -121.374
surface_form: mount oso
instance_of: Mountain
countries: United States
coordinates: lat: 37.6072
lon: -107.494
While other Oregon volcanoes that were heavily glaciated—such as Mount Washington and Mount Thielsen—display eroded volcanic necks, Three Fingered Jack's present summit is a comparatively narrow ridge of loose tephra supported by a dike only thick on a generally north–south axis. Glaciation exposed radiating dikes and plugs that support this summit.

Geographic entities mentioned:
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instance_of: Mountain
countries: United States
coordinates: lat: 43.152837292
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surface_form: washington
instance_of: Lake
countries: United States
coordinates: lat: 47.616666666667
lon: -122.26472222222
surface_form: mount washington
instance_of: Mountain
countries: United States
coordinates: lat: 47.5311964
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surface_form: three fingered jack
instance_of: Mountain
countries: United States
coordinates: lat: 44.478965122
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surface_form: mount washington
instance_of: Mountain
countries: United States
coordinates: lat: 42.1019
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surface_form: mount washington
instance_of: Mountain
countries: United States
coordinates: lat: 38.9149
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surface_form: mount washington
instance_of: Mountain
countries: United States
coordinates: lat: 40.4271
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surface_form: mount washington
instance_of: Mountain
countries: United States
coordinates: lat: 44.270827777778
lon: -71.303483333333
surface_form: mount washington
instance_of: Mountain
countries: United States
coordinates: lat: 44.3321
lon: -121.839
surface_form: mount washington
instance_of: Mountain
countries: United States
coordinates: lat: 47.4259
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Geology and subfeatures. Three Fingered Jack is a shield volcano, and it is part of the group of volcanoes known as Oregon's Matterhorns, whose tall, pinnacle spires resemble the Matterhorn in Switzerland.

Geographic entities mentioned:
surface_form: Matterhorn
instance_of: Mountain
countries: Switzerland
Italy
coordinates: lat: 45.97638888888889
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surface_form: three fingered jack
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countries: United States
coordinates: lat: 44.478965122
lon: -121.843058797
surface_form: matterhorn
instance_of: Mountain
countries: United States
coordinates: lat: 41.8107
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Three Fingered Jack is a shield volcano, and it is part of the group of volcanoes known as Oregon's Matterhorns, whose tall, pinnacle spires resemble the Matterhorn in Switzerland. The volcano (like Mount Thielsen, Mount Bailey, Diamond Peak, and Mount Washington) had a shorter lifespan than larger volcanoes in the Cascade Range, ceasing eruptive activity more than 100,000 years ago.

Geographic entities mentioned:
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instance_of: Mountain
countries: United States
coordinates: lat: 43.152837292
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instance_of: Lake
countries: United States
coordinates: lat: 47.616666666667
lon: -122.26472222222
surface_form: mount washington
instance_of: Mountain
countries: United States
coordinates: lat: 47.5311964
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surface_form: diamond peak
instance_of: Mountain
countries: United States
coordinates: lat: 36.82632
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surface_form: mount bailey
instance_of: Mountain
countries: United States
coordinates: lat: 43.155144764
lon: -122.219995761
surface_form: diamond peak
instance_of: Mountain
countries: United States
coordinates: lat: 40.9503
lon: -108.878
surface_form: diamond peak
instance_of: Mountain
countries: United States
coordinates: lat: 35.76777
lon: -113.35382
surface_form: diamond peak
instance_of: Mountain
countries: United States
coordinates: lat: 43.5207
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surface_form: diamond peak
instance_of: Mountain
countries: United States
coordinates: lat: 44.1417
lon: -113.083
surface_form: mount washington
instance_of: Mountain
countries: United States
coordinates: lat: 42.1019
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surface_form: mount washington
instance_of: Mountain
countries: United States
coordinates: lat: 38.9149
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surface_form: diamond peak
instance_of: Mountain
countries: United States
coordinates: lat: 39.5849
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surface_form: mount washington
instance_of: Mountain
countries: United States
coordinates: lat: 40.4271
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surface_form: mount washington
instance_of: Mountain
countries: United States
coordinates: lat: 44.270827777778
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surface_form: mount washington
instance_of: Mountain
countries: United States
coordinates: lat: 44.3321
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surface_form: mount bailey
instance_of: Mountain
countries: United States
coordinates: lat: 39.4153
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surface_form: mount washington
instance_of: Mountain
countries: United States
coordinates: lat: 47.4259
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During the ongoing Holocene epoch, there has been volcanic activity between the Three Sisters volcanoes and Three Fingered Jack. Such eruptive episodes have produced tephra and lava flows that cover several hundred square kilometers in the region. These eruptions occurred after the climactic eruption of Mount Mazama, which took place roughly 6,600 years ago. Human history.

Geographic entities mentioned:
surface_form: Mount Mazama
instance_of: Mountain
countries: United States
coordinates: lat: 42.9165186
lon: -122.0844711
surface_form: mount mazama
instance_of: Lake
countries: United States
coordinates: lat: 42.943611111111
lon: -122.10666666667
surface_form: mazama
instance_of: Mountain
countries: United States
coordinates: lat: 42.9165186
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state of Oregon, in Linn and Jefferson counties. It has a volume of and a summit elevation of, with a proximal topographic relief of and a draping relief of. Its jagged edifice rises between Mount Jefferson and the Three Sisters volcanic complex. Three Fingered Jack lies within the Mount Jefferson Wilderness and is only accessible on foot by trails such as the Pacific Crest Trail.

Geographic entities mentioned:
surface_form: mount jefferson
instance_of: Mountain
countries: United States
coordinates: lat: 44.6743006
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surface_form: jefferson
instance_of: Mountain
countries: United States
coordinates: lat: 44.6743006
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surface_form: mount jefferson
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countries: United States
coordinates: lat: 45.3522
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countries: United States
coordinates: lat: 42.4584
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countries: United States
coordinates: lat: 38.752
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countries: United States
coordinates: lat: 38.0328
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surface_form: three sisters
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countries: United States
coordinates: lat: 34.5968
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surface_form: mount jefferson
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countries: United States
coordinates: lat: 44.3042
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surface_form: mount jefferson
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countries: United States
coordinates: lat: 42.4918
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surface_form: mount jefferson
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countries: United States
coordinates: lat: 45.6028
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surface_form: mount jefferson
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countries: United States
coordinates: lat: 36.403055555556
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countries: United States
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countries: United States
coordinates: lat: 44.562
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surface_form: three sisters
instance_of: Mountain
countries: United States
coordinates: lat: 33.8697
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Its jagged edifice rises between Mount Jefferson and the Three Sisters volcanic complex. Three Fingered Jack lies within the Mount Jefferson Wilderness and is only accessible on foot by trails such as the Pacific Crest Trail. Located about northwest of the city of Sisters, it is a prominent landmark in the area. Physical geography.

Geographic entities mentioned:
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instance_of: Mountain
countries: United States
coordinates: lat: 44.6743006
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surface_form: jefferson
instance_of: Mountain
countries: United States
coordinates: lat: 44.6743006
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countries: United States
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countries: United States
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countries: United States
coordinates: lat: 38.0328
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countries: United States
coordinates: lat: 44.478965122
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countries: United States
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countries: United States
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countries: United States
coordinates: lat: 45.6028
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surface_form: mount jefferson
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countries: United States
coordinates: lat: 36.403055555556
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surface_form: mount jefferson
instance_of: Mountain
countries: United States
coordinates: lat: 44.562
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Three Fingered Jack marks the northernmost point for this group. South of Mount Jefferson, the High Cascades of Oregon consist of a broad ridge produced by shield volcano activity and eruptions from cinder cones. Vents range from deeply eroded complexes to recently active volcanoes, with most of the region mantled by normally polarized rock produced within the past 730,000 years.

Geographic entities mentioned:
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instance_of: Mountain
countries: United States
coordinates: lat: 44.6743006
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surface_form: jefferson
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countries: United States
coordinates: lat: 44.6743006
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countries: United States
coordinates: lat: 45.3522
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countries: United States
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countries: United States
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countries: United States
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countries: United States
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countries: United States
coordinates: lat: 45.6028
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countries: United States
coordinates: lat: 36.403055555556
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surface_form: mount jefferson
instance_of: Mountain
countries: United States
coordinates: lat: 44.562
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Others allege that the volcano was named after a trapper with less than five fingers on one of his hands. Recreation. Hikers can see Three Fingered Jack on trails surrounding the mountain. The Canyon Creek Meadows hiking trail begins at Jack Lake, progresses through the Mount Jefferson Wilderness, and runs for about. It has an elevation gain of, and is accessible to children and families.

Geographic entities mentioned:
surface_form: mount jefferson
instance_of: Mountain
countries: United States
coordinates: lat: 44.6743006
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surface_form: jefferson
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countries: United States
coordinates: lat: 44.6743006
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countries: United States
coordinates: lat: 44.562
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Three Fingered Jack can still be climbed, but climbers can require rescue after becoming disoriented in low visibility conditions. Geography. Three Fingered Jack lies in the U.S. state of Oregon, in Linn and Jefferson counties. It has a volume of and a summit elevation of, with a proximal topographic relief of and a draping relief of.

Geographic entities mentioned:
surface_form: jefferson
instance_of: Mountain
countries: United States
coordinates: lat: 44.6743006
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surface_form: three fingered jack
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countries: United States
coordinates: lat: 44.478965122
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It has an elevation gain of, and is accessible to children and families. An additional connected hiking trail runs for another up the rocky glacial washout plain adjacent to the volcano, becoming steeper as it approaches Three Fingered Jack and gaining in elevation. The base can also be reached on Pacific Crest Trail which runs for round trip and offers views of the volcano and its summit lake.

Geographic entities mentioned:
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countries: United States
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countries: United States
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coordinates: lat: 60.6313
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Other shield volcanoes and cinder cones that were active during the Pleistocene epoch occur to the northwest and southwest. The volcano has a long ridge that trends from north to south. It is highly eroded; shaped like a sawtooth, it consists of tephra deposits supported by a vertical dike with a thickness of. Erosion has been so extensive that climbers claim that the summit moves in the wind.

Geographic entities mentioned:
surface_form: long ridge
instance_of: Mountain
countries: United States
coordinates: lat: 37.2819
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It is likely stagnant. During the Little Ice Age, which spanned roughly 1350 to 1850, the glacier produced moraines with heights close to, which are dotted with of ash from the Sand Mountain cinder cone chain and of ash from the Blue Lake Crater cinder cone. The moraine for Jack Glacier dammed a lake with a volume of, a surface area of, and a maximum depth of.

Geographic entities mentioned:
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countries: United States
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