Sarmila/GeoWiki-Features huggingface dataset:
It has ten lakes, connected by a series of canals. The ten lakes on the northern chain are Lake Haines, Lake Rochelle, Lake Echo, Lake Conine, Lake Fannie, Lake Smart, Lake Henry, Lake Hamilton, Middle Lake Hamilton, and Little Lake Hamilton. The southern chain is located almost entirely within the city of Winter Haven. It has 16, sometimes 18, lakes connected by a series of canals.

Geographic entities mentioned:
surface_form: Lake Rochelle
instance_of: Lake
countries: United States
coordinates: lat: 28.0728
lon: -81.7215
surface_form: Lake Conine
instance_of: Lake
countries: United States
coordinates: lat: 28.06
lon: -81.7251
surface_form: Lake Fannie
instance_of: Lake
countries: United States
coordinates: lat: 28.0603
lon: -81.6895
surface_form: Lake Smart
instance_of: Lake
countries: United States
coordinates: lat: 28.0589
lon: -81.7109
surface_form: Middle Lake Hamilton
instance_of: Lake
countries: United States
coordinates: lat: 28.0697
lon: -81.6479
surface_form: Little Lake Hamilton
instance_of: Lake
countries: United States
coordinates: lat: 28.072
lon: -81.6345
It has 16, sometimes 18, lakes connected by a series of canals. The principal 16 lakes on the southern chain are Lake Howard, Lake Cannon, Lake Shipp, Lake Jessie, Lake Hartridge, Lake Lulu, Lake Roy, Lake Eloise, Little Lake Eloise, Lake Winterset, Little Lake Winterset, Lake May, Lake Mirror, Lake Idylwild, Spring Lake and Lake Summit. Hydrography.

Geographic entities mentioned:
surface_form: Lake Cannon
instance_of: Lake
countries: United States
coordinates: lat: 28.0389
lon: -81.7526
surface_form: Lake Shipp
instance_of: Lake
countries: United States
coordinates: lat: 28.0039
lon: -81.7423
surface_form: Lake Hartridge
instance_of: Lake
countries: United States
coordinates: lat: 28.0567
lon: -81.7429
surface_form: Lake Lulu
instance_of: Lake
countries: United States
coordinates: lat: 27.9964
lon: -81.7209
surface_form: Lake Eloise
instance_of: Lake
countries: United States
coordinates: lat: 27.9836
lon: -81.704
surface_form: Lake Winterset
instance_of: Lake
countries: United States
coordinates: lat: 27.9745
lon: -81.682
surface_form: Lake Idylwild
instance_of: Lake
countries: United States
coordinates: lat: 28.0503
lon: -81.7567
surface_form: Lake Summit
instance_of: Lake
countries: United States
coordinates: lat: 27.9988
lon: -81.6948
The area had no European or American settlement until the Florida Armed Occupation Act of 1842, which created incentives for settlers. Some of the lakes on the chain were named by these early settlers, including Lake Eloise, named for the daughter of the first American settler on that lake. During the 1840s and 1850s, the United States government conducted the first surveys of the area.

Geographic entities mentioned:
surface_form: Lake Eloise
instance_of: Lake
countries: United States
coordinates: lat: 27.9836
lon: -81.704
Porretta Terme is located about south-west of Bologna. Known since Roman times for its thermal springs, it is also a center for winter sports thanks to the nearby resorts of Corno alle Scale, Abetone, Monte Cimone. It was a separate &quot;comune&quot; until January 2016, when it merged with Granaglione to form the new comune of Alto Reno Terme.

Geographic entities mentioned:
surface_form: Monte Cimone
instance_of: Mountain
countries: Italy
coordinates: lat: 44.193888888889
lon: 10.701388888889
The 15th Scottish Infantry Division joined the Corps on the 4th April. The following weeks were filled with many short but intense battles and fighting across Northern Germany. The Corps crossed the Elbe at midnight 30 April advanced north east and occupied Plön in Schleswig-Holstein. The fighting continued until the unconditional surrender by German forces on the 7th May 1945.

Geographic entities mentioned:
surface_form: Elbe
instance_of: Watercourse
countries: Czech Republic
Germany
coordinates: lat: 53.922222222222224
lon: 8.722222222222221
Exile Hill. Exile Hill, sometimes referred to as Exile Peak, is an isolated hill in Cassiar Land District of northwestern British Columbia, Canada. It has an elevation of and is part of the Arctic Lake Plateau or the neighbouring Spectrum Range, which are within the limits of the Tahltan Highland. Exile Hill is about southeast of the community of Telegraph Creek in Mount Edziza Provincial Park.

Geographic entities mentioned:
surface_form: Arctic Lake Plateau
instance_of: Plateau
countries: Canada
coordinates: lat: 57.3
lon: -130.767
It has an elevation of and is part of the Arctic Lake Plateau or the neighbouring Spectrum Range, which are within the limits of the Tahltan Highland. Exile Hill is about southeast of the community of Telegraph Creek in Mount Edziza Provincial Park. Access to Exile Hill is via aircraft, which are permitted to land on Mess Lake and Little Arctic Lake to the northwest and southeast, respectively.

Geographic entities mentioned:
surface_form: Mess Lake
instance_of: Lake
countries: Canada
coordinates: lat: 57.4667
lon: -130.883
surface_form: exile hill
instance_of: Mountain
countries: Canada
coordinates: lat: 57.3783
lon: -130.825
Access to Exile Hill is via aircraft, which are permitted to land on Mess Lake and Little Arctic Lake to the northwest and southeast, respectively. Exile Hill is part of the Mount Edziza volcanic complex, which consists of diverse landforms such as shield volcanoes, stratovolcanoes, lava domes and cinder cones.

Geographic entities mentioned:
surface_form: Mount Edziza volcanic complex
instance_of: Mountain
countries: Canada
coordinates: lat: 57.5
lon: -130.6
surface_form: edziza
instance_of: Mountain
countries: Canada
coordinates: lat: 57.715555555555554
lon: -130.63472222222222
surface_form: mount edziza
instance_of: Mountain
countries: Canada
coordinates: lat: 57.715555555555554
lon: -130.63472222222222
surface_form: exile hill
instance_of: Mountain
countries: Canada
coordinates: lat: 57.3783
lon: -130.825
Basalt comprises the Nido Formation whereas the younger Spectrum Formation consists of trachyte. Nearby volcanic features include Outcast Hill, Tadekho Hill, Kuno Peak, Nahta Cone and Wetalth Ridge. Name and etymology.

Geographic entities mentioned:
surface_form: Outcast Hill
instance_of: Mountain
countries: Canada
coordinates: lat: 57.39
lon: -130.774
surface_form: Tadekho Hill
instance_of: Mountain
countries: Canada
coordinates: lat: 57.3503
lon: -130.785
surface_form: Kuno Peak
instance_of: Mountain
countries: Canada
coordinates: lat: 57.3763
lon: -130.7398
surface_form: Nahta Cone
instance_of: Mountain
countries: Canada
coordinates: lat: 57.3083
lon: -130.821
surface_form: Wetalth Ridge
instance_of: Mountain
countries: Canada
coordinates: lat: 57.2275
lon: -130.786
&quot;Exile&quot; is a reference to the Wetalth, a group of seven people previously living in the area who were exiled or outcasted from the Tahltans. Nahta Cone, Outcast Hill and Wetalth Ridge are extensions of the Wetalth theme.

Geographic entities mentioned:
surface_form: Nahta Cone
instance_of: Mountain
countries: Canada
coordinates: lat: 57.3083
lon: -130.821
surface_form: Outcast Hill
instance_of: Mountain
countries: Canada
coordinates: lat: 57.39
lon: -130.774
surface_form: Wetalth Ridge
instance_of: Mountain
countries: Canada
coordinates: lat: 57.2275
lon: -130.786
surface_form: outcast hill
instance_of: Mountain
countries: Canada
coordinates: lat: 57.39
lon: -130.774
surface_form: wetalth ridge
instance_of: Mountain
countries: Canada
coordinates: lat: 57.2275
lon: -130.786
Geography. Exile Hill is located about southeast of the community of Telegraph Creek in Cassiar Land District of northwestern British Columbia, Canada. It has an elevation of and is part of the Arctic Lake Plateau or the neighbouring Spectrum Range, which are at the southern end of the Mount Edziza volcanic complex.

Geographic entities mentioned:
surface_form: Arctic Lake Plateau
instance_of: Plateau
countries: Canada
coordinates: lat: 57.3
lon: -130.767
surface_form: Mount Edziza volcanic complex
instance_of: Mountain
countries: Canada
coordinates: lat: 57.5
lon: -130.6
surface_form: mount edziza volcanic complex
instance_of: Mountain
countries: Canada
coordinates: lat: 57.5
lon: -130.6
surface_form: edziza
instance_of: Mountain
countries: Canada
coordinates: lat: 57.715555555555554
lon: -130.63472222222222
surface_form: mount edziza
instance_of: Mountain
countries: Canada
coordinates: lat: 57.715555555555554
lon: -130.63472222222222
surface_form: arctic lake plateau
instance_of: Plateau
countries: Canada
coordinates: lat: 57.3
lon: -130.767
The volcanic complex consists of a group of overlapping shield volcanoes, stratovolcanoes, lava domes and cinder cones that have formed over the last 7.5 million years. Exile Hill rises above the southeastern side of Mess Creek valley and is topographically higher than its surroundings. The terrain east of Exile Hill is relatively flat, but elsewhere it is surrounded by vegetated valleys.

Geographic entities mentioned:
surface_form: Mess Creek
instance_of: Watercourse
countries: Canada
coordinates: lat: 57.88296
lon: -131.2206
surface_form: mess creek
instance_of: Watercourse
countries: Canada
coordinates: lat: 57.88296
lon: -131.2206
surface_form: exile hill
instance_of: Mountain
countries: Canada
coordinates: lat: 57.3783
lon: -130.825
The terrain east of Exile Hill is relatively flat, but elsewhere it is surrounded by vegetated valleys. Tadekho Creek and Nahta Creek flow through valleys north and south of Exile Hill, respectively, and are tributaries of Mess Creek. Exile Hill is surrounded by a number of other landforms within the Mount Edziza volcanic complex.

Geographic entities mentioned:
surface_form: Tadekho Creek
instance_of: Watercourse
countries: Canada
coordinates: lat: 57.43296
lon: -130.90399
surface_form: mess creek
instance_of: Watercourse
countries: Canada
coordinates: lat: 57.88296
lon: -131.2206
surface_form: exile hill
instance_of: Mountain
countries: Canada
coordinates: lat: 57.3783
lon: -130.825
surface_form: exile hill
instance_of: Mountain
countries: Canada
coordinates: lat: 57.3783
lon: -130.825
Exile Hill is surrounded by a number of other landforms within the Mount Edziza volcanic complex. Outcast Hill, about to the northeast, is a cinder cone on an interfluve between Tadekho Creek to the south and an unnamed tributary of Tadekho Creek to the north. About southeast of Exile Hill is Tadekho Hill, a nearly circular volcanic cone about northwest of Little Arctic Lake.

Geographic entities mentioned:
surface_form: Tadekho Hill
instance_of: Mountain
countries: Canada
coordinates: lat: 57.3503
lon: -130.785
surface_form: tadekho hill
instance_of: Mountain
countries: Canada
coordinates: lat: 57.3503
lon: -130.785
About southeast of Exile Hill is Tadekho Hill, a nearly circular volcanic cone about northwest of Little Arctic Lake. Kuno Peak, about to the east, is a glaciated mountain peak at the western end of a ridge extending from the southwestern end of the Spectrum Range.

Geographic entities mentioned:
surface_form: Kuno Peak
instance_of: Mountain
countries: Canada
coordinates: lat: 57.3763
lon: -130.7398
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
Exile Hill lies in Mount Edziza Provincial Park which, with an area of, is one of the largest provincial parks in British Columbia. It was established in 1972 to showcase the volcanic landscape extending from Mount Edziza in the north to the Spectrum Range in the south.

Geographic entities mentioned:
surface_form: Mount Edziza
instance_of: Mountain
countries: Canada
coordinates: lat: 57.715555555555554
lon: -130.63472222222222
surface_form: edziza
instance_of: Mountain
countries: Canada
coordinates: lat: 57.715555555555554
lon: -130.63472222222222
surface_form: edziza
instance_of: Mountain
countries: Canada
coordinates: lat: 57.715555555555554
lon: -130.63472222222222
surface_form: mount edziza
instance_of: Mountain
countries: Canada
coordinates: lat: 57.715555555555554
lon: -130.63472222222222
surface_form: mount edziza
instance_of: Mountain
countries: Canada
coordinates: lat: 57.715555555555554
lon: -130.63472222222222
It was established in 1972 to showcase the volcanic landscape extending from Mount Edziza in the north to the Spectrum Range in the south. Mount Edziza Provincial Park is in the Tahltan Highland, a southeast-trending upland area extending along the western side of the Stikine Plateau. Background.

Geographic entities mentioned:
surface_form: Stikine Plateau
instance_of: Plateau
countries: Canada
coordinates: lat: 58.38305555555556
lon: -129.885
surface_form: stikine plateau
instance_of: Plateau
countries: Canada
coordinates: lat: 58.38305555555556
lon: -129.885
Background. As a part of the Mount Edziza volcanic complex, Exile Hill lies within a broad area of volcanoes and lava flows called the Northern Cordilleran Volcanic Province, which extends from northwestern British Columbia northwards through Yukon into easternmost Alaska.

Geographic entities mentioned:
surface_form: Northern Cordilleran Volcanic Province
instance_of: Mountain
countries: Canada
coordinates: lat: 57.7156
lon: -130.634
surface_form: columbia
instance_of: Mountain
countries: Canada
coordinates: lat: 52.1475
lon: -117.44055555555556
surface_form: northern cordilleran volcanic province
instance_of: Mountain
countries: Canada
coordinates: lat: 57.7156
lon: -130.634
surface_form: exile hill
instance_of: Mountain
countries: Canada
coordinates: lat: 57.3783
lon: -130.825
The breccia was deposited by an explosive eruption and consists of immensely altered, rusty trachyte clasts in a yellowish-brown groundmass of much smaller breccia particles. Yeda Peak about east of Exile Hill was the site of a similar but much larger eruption near the end of the Spectrum eruptive period.

Geographic entities mentioned:
surface_form: Yeda Peak
instance_of: Mountain
countries: Canada
coordinates: lat: 57.3811
lon: -130.678
As of 2025, Alpine Lakes Air and BC Yukon Air are the only air charter companies permitted to provide access to this area via aircraft. Private aircraft are also permitted to land in the area, but a letter of authorization from the BC Parks Stikine Senior Park Ranger is required to land on Mess Lake and Little Arctic Lake, which are the closest lakes of significant size to Exile Hill.

Geographic entities mentioned:
surface_form: Mess Lake
instance_of: Lake
countries: Canada
coordinates: lat: 57.4667
lon: -130.883
surface_form: exile hill
instance_of: Mountain
countries: Canada
coordinates: lat: 57.3783
lon: -130.825
surface_form: mess lake
instance_of: Lake
countries: Canada
coordinates: lat: 57.4667
lon: -130.883
A series of basaltic lava flows up to thick, believed to have originated from a vent adjacent to Exile Hill, are exposed in isolated buttes and in cliffs along the upper Mess Creek valley. Basaltic lava flows of Exile Hill are geomorphologically and compositionally more diverse than those from the Swarm Peak and Vanished Peak eruptive centres.

Geographic entities mentioned:
surface_form: mess creek
instance_of: Watercourse
countries: Canada
coordinates: lat: 57.88296
lon: -131.2206
surface_form: exile hill
instance_of: Mountain
countries: Canada
coordinates: lat: 57.3783
lon: -130.825
surface_form: exile hill
instance_of: Mountain
countries: Canada
coordinates: lat: 57.3783
lon: -130.825
Exile Hill. Exile Hill, sometimes referred to as Exile Peak, is an isolated hill in Cassiar Land District of northwestern British Columbia, Canada. It has an elevation of and is part of the Arctic Lake Plateau or the neighbouring Spectrum Range, which are within the limits of the Tahltan Highland. Exile Hill is about southeast of the community of Telegraph Creek in Mount Edziza Provincial Park.

Geographic entities mentioned:
surface_form: columbia
instance_of: Mountain
countries: Canada
coordinates: lat: 52.1475
lon: -117.44055555555556
surface_form: exile hill
instance_of: Mountain
countries: Canada
coordinates: lat: 57.3783
lon: -130.825
Nahta Cone, Outcast Hill and Wetalth Ridge are extensions of the Wetalth theme. Canadian volcanologist Jack Souther labelled Exile Hill as &quot;Exile Peak&quot; on a geological map in his 1992 report, &quot;The Late Cenozoic Mount Edziza Volcanic Complex, British Columbia&quot;. Geography.

Geographic entities mentioned:
surface_form: columbia
instance_of: Mountain
countries: Canada
coordinates: lat: 52.1475
lon: -117.44055555555556
surface_form: mount edziza volcanic complex
instance_of: Mountain
countries: Canada
coordinates: lat: 57.5
lon: -130.6
surface_form: edziza
instance_of: Mountain
countries: Canada
coordinates: lat: 57.715555555555554
lon: -130.63472222222222
surface_form: mount edziza
instance_of: Mountain
countries: Canada
coordinates: lat: 57.715555555555554
lon: -130.63472222222222
surface_form: exile hill
instance_of: Mountain
countries: Canada
coordinates: lat: 57.3783
lon: -130.825
surface_form: exile hill
instance_of: Mountain
countries: Canada
coordinates: lat: 57.3783
lon: -130.825
Geography. Exile Hill is located about southeast of the community of Telegraph Creek in Cassiar Land District of northwestern British Columbia, Canada. It has an elevation of and is part of the Arctic Lake Plateau or the neighbouring Spectrum Range, which are at the southern end of the Mount Edziza volcanic complex.

Geographic entities mentioned:
surface_form: columbia
instance_of: Mountain
countries: Canada
coordinates: lat: 52.1475
lon: -117.44055555555556
About south and southeast of Exile Hill are Nahta Cone and Wetalth Ridge, respectively, which are on the opposite side of Nahta Creek valley. Exile Hill lies in Mount Edziza Provincial Park which, with an area of, is one of the largest provincial parks in British Columbia.

Geographic entities mentioned:
surface_form: columbia
instance_of: Mountain
countries: Canada
coordinates: lat: 52.1475
lon: -117.44055555555556
Exile Hill is part of the Mount Edziza volcanic complex, which consists of diverse landforms such as shield volcanoes, stratovolcanoes, lava domes and cinder cones. The volcanic rocks comprising the hill are of Pliocene age and are subdivided into two geological formations that were deposited during the second magmatic cycle of the Mount Edziza volcanic complex.

Geographic entities mentioned:
surface_form: mount edziza volcanic complex
instance_of: Mountain
countries: Canada
coordinates: lat: 57.5
lon: -130.6
surface_form: edziza
instance_of: Mountain
countries: Canada
coordinates: lat: 57.715555555555554
lon: -130.63472222222222
surface_form: mount edziza
instance_of: Mountain
countries: Canada
coordinates: lat: 57.715555555555554
lon: -130.63472222222222
Tadekho Creek and Nahta Creek flow through valleys north and south of Exile Hill, respectively, and are tributaries of Mess Creek. Exile Hill is surrounded by a number of other landforms within the Mount Edziza volcanic complex. Outcast Hill, about to the northeast, is a cinder cone on an interfluve between Tadekho Creek to the south and an unnamed tributary of Tadekho Creek to the north.

Geographic entities mentioned:
surface_form: mount edziza volcanic complex
instance_of: Mountain
countries: Canada
coordinates: lat: 57.5
lon: -130.6
surface_form: edziza
instance_of: Mountain
countries: Canada
coordinates: lat: 57.715555555555554
lon: -130.63472222222222
surface_form: mount edziza
instance_of: Mountain
countries: Canada
coordinates: lat: 57.715555555555554
lon: -130.63472222222222
Stratigraphy. Exile Hill consists of Pliocene volcanic rocks that comprise two geological formations, both of which were deposited by volcanic eruptions during the second magmatic cycle of the Mount Edziza volcanic complex.

Geographic entities mentioned:
surface_form: mount edziza volcanic complex
instance_of: Mountain
countries: Canada
coordinates: lat: 57.5
lon: -130.6
surface_form: edziza
instance_of: Mountain
countries: Canada
coordinates: lat: 57.715555555555554
lon: -130.63472222222222
surface_form: mount edziza
instance_of: Mountain
countries: Canada
coordinates: lat: 57.715555555555554
lon: -130.63472222222222
Exile Hill is the only eruptive centre of the Mount Edziza volcanic complex known to have been active during both the Nido and Spectrum eruptive periods, but the amount of lava erupted from it remains unknown. Nido Formation. The formation of Exile Hill began with the eruption of a small cinder cone on the extreme western edge of the surrounding plateau.

Geographic entities mentioned:
surface_form: mount edziza volcanic complex
instance_of: Mountain
countries: Canada
coordinates: lat: 57.5
lon: -130.6
surface_form: edziza
instance_of: Mountain
countries: Canada
coordinates: lat: 57.715555555555554
lon: -130.63472222222222
surface_form: mount edziza
instance_of: Mountain
countries: Canada
coordinates: lat: 57.715555555555554
lon: -130.63472222222222
Kuno Peak, about to the east, is a glaciated mountain peak at the western end of a ridge extending from the southwestern end of the Spectrum Range. About south and southeast of Exile Hill are Nahta Cone and Wetalth Ridge, respectively, which are on the opposite side of Nahta Creek valley.

Geographic entities mentioned:
surface_form: nahta cone
instance_of: Mountain
countries: Canada
coordinates: lat: 57.3083
lon: -130.821
surface_form: wetalth ridge
instance_of: Mountain
countries: Canada
coordinates: lat: 57.2275
lon: -130.786
surface_form: exile hill
instance_of: Mountain
countries: Canada
coordinates: lat: 57.3783
lon: -130.825
Exile Hill is surrounded by a number of other landforms within the Mount Edziza volcanic complex. Outcast Hill, about to the northeast, is a cinder cone on an interfluve between Tadekho Creek to the south and an unnamed tributary of Tadekho Creek to the north. About southeast of Exile Hill is Tadekho Hill, a nearly circular volcanic cone about northwest of Little Arctic Lake.

Geographic entities mentioned:
surface_form: tadekho creek
instance_of: Watercourse
countries: Canada
coordinates: lat: 57.43296
lon: -130.90399
surface_form: tadekho creek
instance_of: Watercourse
countries: Canada
coordinates: lat: 57.43296
lon: -130.90399
surface_form: cinder cone
instance_of: Mountain
countries: Canada
coordinates: lat: 49.9717
lon: -123.007
Nido Formation. The formation of Exile Hill began with the eruption of a small cinder cone on the extreme western edge of the surrounding plateau. This cone was almost completely inundated by younger lava flows from the south and east, but thick deposits of bombs and agglutinated spatter exposed on the southeastern flank of Exile Hill are probably remnants of this early cone.

Geographic entities mentioned:
surface_form: cinder cone
instance_of: Mountain
countries: Canada
coordinates: lat: 49.9717
lon: -123.007
It has an elevation of and is part of the Arctic Lake Plateau or the neighbouring Spectrum Range, which are within the limits of the Tahltan Highland. Exile Hill is about southeast of the community of Telegraph Creek in Mount Edziza Provincial Park. Access to Exile Hill is via aircraft, which are permitted to land on Mess Lake and Little Arctic Lake to the northwest and southeast, respectively.

Geographic entities mentioned:
surface_form: edziza
instance_of: Mountain
countries: Canada
coordinates: lat: 57.715555555555554
lon: -130.63472222222222
surface_form: mount edziza
instance_of: Mountain
countries: Canada
coordinates: lat: 57.715555555555554
lon: -130.63472222222222
surface_form: exile hill
instance_of: Mountain
countries: Canada
coordinates: lat: 57.3783
lon: -130.825
Exile Hill. Exile Hill, sometimes referred to as Exile Peak, is an isolated hill in Cassiar Land District of northwestern British Columbia, Canada. It has an elevation of and is part of the Arctic Lake Plateau or the neighbouring Spectrum Range, which are within the limits of the Tahltan Highland. Exile Hill is about southeast of the community of Telegraph Creek in Mount Edziza Provincial Park.

Geographic entities mentioned:
surface_form: exile hill
instance_of: Mountain
countries: Canada
coordinates: lat: 57.3783
lon: -130.825
Exile Hill consists of Pliocene volcanic rocks that comprise two geological formations, both of which were deposited by volcanic eruptions during the second magmatic cycle of the Mount Edziza volcanic complex. The oldest geological formation, the 4.4-million-year-old Nido Formation, is subdivided into two geological members; the Kounugu Member is the main geological member at Exile Hill.

Geographic entities mentioned:
surface_form: exile hill
instance_of: Mountain
countries: Canada
coordinates: lat: 57.3783
lon: -130.825
The oldest geological formation, the 4.4-million-year-old Nido Formation, is subdivided into two geological members; the Kounugu Member is the main geological member at Exile Hill. Alkali basalt, hawaiite and picrite are the main rocks comprising the Kounugu Member, which erupted from at least four separate eruptive centres: Swarm Peak, Vanished Peak, Lost Peak and Exile Hill.

Geographic entities mentioned:
surface_form: exile hill
instance_of: Mountain
countries: Canada
coordinates: lat: 57.3783
lon: -130.825
The youngest geological formation, the 3.1-million-year-old Spectrum Formation, comprises mostly comendite, pantellerite and pantelleritic trachyte that erupted from the Spectrum Dome and much smaller satellitic centres such as Exile Hill.

Geographic entities mentioned:
surface_form: exile hill
instance_of: Mountain
countries: Canada
coordinates: lat: 57.3783
lon: -130.825
surface_form: exile hill
instance_of: Mountain
countries: Canada
coordinates: lat: 57.3783
lon: -130.825
Nido Formation. The formation of Exile Hill began with the eruption of a small cinder cone on the extreme western edge of the surrounding plateau. This cone was almost completely inundated by younger lava flows from the south and east, but thick deposits of bombs and agglutinated spatter exposed on the southeastern flank of Exile Hill are probably remnants of this early cone.

Geographic entities mentioned:
surface_form: exile hill
instance_of: Mountain
countries: Canada
coordinates: lat: 57.3783
lon: -130.825
Basaltic lava flows of Exile Hill are geomorphologically and compositionally more diverse than those from the Swarm Peak and Vanished Peak eruptive centres. The lowermost basaltic lava flow forming the base of Exile Hill is more than thick whereas the uppermost rubbly basaltic lava flows are only a few metres in thickness.

Geographic entities mentioned:
surface_form: exile hill
instance_of: Mountain
countries: Canada
coordinates: lat: 57.3783
lon: -130.825
Yeda Peak about east of Exile Hill was the site of a similar but much larger eruption near the end of the Spectrum eruptive period. A roughly thick series of trachyte lava flows caps the summit of Exile Hill and overlies the thick layer of gravel capping the Nido Formation basalt. The trachyte is fine grained, pantelleritic in composition and contains wide phenocrysts of feldspar.

Geographic entities mentioned:
surface_form: exile hill
instance_of: Mountain
countries: Canada
coordinates: lat: 57.3783
lon: -130.825
The trachyte is fine grained, pantelleritic in composition and contains wide phenocrysts of feldspar. Interlayering these lava flows are beds of pyroclastic material containing bombs, spatter and light-coloured trachyte blocks that have been fused together. Exposed on the southwestern side of Exile Hill is a small porous green trachyte intrusion underlying the breccia.

Geographic entities mentioned:
surface_form: exile hill
instance_of: Mountain
countries: Canada
coordinates: lat: 57.3783
lon: -130.825
Basement. Exile Hill is underlain by metasedimentary rocks of the Stikinia terrane, a Paleozoic and Mesozoic suite of volcanic and sedimentary rocks that accreted to the continental margin of North America during the Jurassic. Most of these rocks around the base of Exile Hill are covered with felsenmeer, till, glacial outwash, fluvial outwash or solifluction deposits.

Geographic entities mentioned:
surface_form: exile hill
instance_of: Mountain
countries: Canada
coordinates: lat: 57.3783
lon: -130.825
surface_form: exile hill
instance_of: Mountain
countries: Canada
coordinates: lat: 57.3783
lon: -130.825
Private aircraft are also permitted to land in the area, but a letter of authorization from the BC Parks Stikine Senior Park Ranger is required to land on Mess Lake and Little Arctic Lake, which are the closest lakes of significant size to Exile Hill. These two lakes are about northwest and southeast of Exile Hill, respectively.

Geographic entities mentioned:
surface_form: exile hill
instance_of: Mountain
countries: Canada
coordinates: lat: 57.3783
lon: -130.825
Pseudocrenilabrus pyrrhocaudalis. &quot;Pseudocrenilabrus pyrrhocaudalis&quot;, the fire-tailed pseudocrenilabrus, is a newly described species of small mouth-brooding haplochromine cichlid from Lake Mweru in south west central Africa.

Geographic entities mentioned:
surface_form: Lake Mweru
instance_of: Lake
countries: Zambia
Democratic Republic of the Congo
coordinates: lat: -9.1666666666667
lon: 28.5
Tempisque River. The Tempisque River, or Río Tempisque, is long, located entirely in Costa Rica flowing from the Guanacaste Cordillera near the Orosí Volcano and emptying into the Gulf of Nicoya. It passes through the Palo Verde National Park and is an important habitat for various species of crocodiles, monkeys, iguanas and birds.

Geographic entities mentioned:
surface_form: Orosí Volcano
instance_of: Mountain
countries: Costa Rica
coordinates: lat: 10.98
lon: -85.473333333333
In 2006, leaked cables from an American diplomat recounted a lavish wedding attended by Kadyrov in Russia's Caucasus region in which guests threw $100 bills at child dancers, and which had nighttime &quot;water-scooter jaunts on the Caspian Sea&quot;, and a report that Kadyrov gave the newly married couple a &quot;five-kilo lump of gold&quot;.

Geographic entities mentioned:
surface_form: Caspian Sea
instance_of: Body of water
Lake
countries: Iran
Russia
Kazakhstan
Azerbaijan
Turkmenistan
Russian Empire
Soviet Union
coordinates: lat: 42
lon: 50.5
As there was no male heir the greater part of Bromley's property ultimately passed to Margaret. Descendants. Margaret Bromley married Sir Richard Newport, an important local landowner whose seat at High Ercall Hall lay just to the north-east of Wroxeter, in sight of the Wrekin. Margaret and Richard Newport had four sons, of whom two died in infancy, and three or four daughters.

Geographic entities mentioned:
surface_form: the Wrekin
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 52.66916666666667
lon: -2.551388888888889
The mountain, as well as its surrounding land-forms, is geographically close to the volcanic caldera at the center of Faial. The eruptive igneous rocks produced by this caldera forms the base of Tambroso, as well as many other peaks on Faial Island. The whole series of peaks has a maximum elevation at Cabeço Gordo, which is above sea level. Geography and geology.

Geographic entities mentioned:
surface_form: Cabeço Gordo
instance_of: Mountain
countries: Portugal
coordinates: lat: 38.585555555556
lon: -28.714444444444
Tambroso. Tambroso is a mountain peak on the Azorian island of Faial. It is located in the civil parish of Ribeirinha, in the municipality of Horta. The mountain, as well as its surrounding land-forms, is geographically close to the volcanic caldera at the center of Faial. The eruptive igneous rocks produced by this caldera forms the base of Tambroso, as well as many other peaks on Faial Island.

Geographic entities mentioned:
surface_form: tambroso
instance_of: Mountain
countries: Portugal
coordinates: lat: 38.59999722
lon: -28.65
Tambroso. Tambroso is a mountain peak on the Azorian island of Faial. It is located in the civil parish of Ribeirinha, in the municipality of Horta. The mountain, as well as its surrounding land-forms, is geographically close to the volcanic caldera at the center of Faial. The eruptive igneous rocks produced by this caldera forms the base of Tambroso, as well as many other peaks on Faial Island.

Geographic entities mentioned:
surface_form: tambroso
instance_of: Mountain
countries: Portugal
coordinates: lat: 38.59999722
lon: -28.65
surface_form: faial
instance_of: Mountain
countries: Portugal
coordinates: lat: 38.585555555556
lon: -28.714444444444
The mountain, as well as its surrounding land-forms, is geographically close to the volcanic caldera at the center of Faial. The eruptive igneous rocks produced by this caldera forms the base of Tambroso, as well as many other peaks on Faial Island. The whole series of peaks has a maximum elevation at Cabeço Gordo, which is above sea level. Geography and geology.

Geographic entities mentioned:
surface_form: tambroso
instance_of: Mountain
countries: Portugal
coordinates: lat: 38.59999722
lon: -28.65
surface_form: faial
instance_of: Mountain
countries: Portugal
coordinates: lat: 38.585555555556
lon: -28.714444444444
The whole series of peaks has a maximum elevation at Cabeço Gordo, which is above sea level. Geography and geology. The elevation of Tambroso itself reaches to above sea-level. It is situated near another local peak, Alto da Pedreira, and the town of Ribeirinha. Climatically, the mountain is situated in a temperate ocean climate, as is the rest of Faial Island.

Geographic entities mentioned:
surface_form: tambroso
instance_of: Mountain
countries: Portugal
coordinates: lat: 38.59999722
lon: -28.65
The area around the base of Tambroso may also be affected by uplift and other types crustal movement along an east-west trending fault which is situation to the south of the mountain.

Geographic entities mentioned:
surface_form: tambroso
instance_of: Mountain
countries: Portugal
coordinates: lat: 38.59999722
lon: -28.65
Tambroso. Tambroso is a mountain peak on the Azorian island of Faial. It is located in the civil parish of Ribeirinha, in the municipality of Horta. The mountain, as well as its surrounding land-forms, is geographically close to the volcanic caldera at the center of Faial. The eruptive igneous rocks produced by this caldera forms the base of Tambroso, as well as many other peaks on Faial Island.

Geographic entities mentioned:
surface_form: faial
instance_of: Mountain
countries: Portugal
coordinates: lat: 38.585555555556
lon: -28.714444444444
It is situated near another local peak, Alto da Pedreira, and the town of Ribeirinha. Climatically, the mountain is situated in a temperate ocean climate, as is the rest of Faial Island. The rocks that make up much of the Azores are generally related to a triple junction which produces Neogene-aged, intrusive and eruptive, mafic igneous rocks, and sedimentary formations derived from them.

Geographic entities mentioned:
surface_form: faial
instance_of: Mountain
countries: Portugal
coordinates: lat: 38.585555555556
lon: -28.714444444444
The rocks that form Tamborso are mapped as part of the Cedros volcanic complex. The lower portion of this volcanic complex's formation began in the middle Pleistocene's Chibanian age, while upper portion consists mainly of pyroclastic flows and other deposits that date from the late Pleistocene up to the year 1958, which marked the most recent eruption on Faial Island.

Geographic entities mentioned:
surface_form: faial
instance_of: Mountain
countries: Portugal
coordinates: lat: 38.585555555556
lon: -28.714444444444
In 2022 the tram tracks were extended south down High Street at a cost of, though due to an engineering issue they derailed a tram and had to be relaid. There is a cable car system called the Christchurch Gondola which operates as a tourist attraction, providing transport from the Heathcote Valley to the top of Mount Cavendish in the city's south-east.

Geographic entities mentioned:
surface_form: Mount Cavendish
instance_of: Mountain
countries: New Zealand
coordinates: lat: -43.5894
lon: 172.7159
Its modern borders are defined, approximately, as being Leith Walk in the south east, Broughton Street in the south west, Broughton Road in the north west and McDonald Road in the north east. Moving clockwise from south east, Broughton is bordered by Greenside and Calton, the New Town, Canonmills, and Pilrig. Broughton Street. Broughton's main thoroughfare is Broughton Street.

Geographic entities mentioned:
surface_form: Calton
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 55.955278
lon: -3.182222
Rosstrappe Chair Lift. The Rosstrappe Chair Lift () is a 559-metre-long single-seater chairlift built in 1980 by the firm of Chrudrim. It runs from Thale in the Bode Gorge taking eight minutes to reach the rock massif of the Roßtrappe. The Rosstrappe Chair Lift climbs 250 metres over a length of 668 metres. It has over 13 supports. In 2005, the old chairlift was replaced by a new one.

Geographic entities mentioned:
surface_form: Bode Gorge
instance_of: Valley
countries: Germany
coordinates: lat: 51.735555555556
lon: 11.009722222222
Eastern brook trout only inhabit Trout Creek. Geology. In southern Washington state, the Cascade Range sits south of the dacitic volcanic belt running from Mount Garibaldi to Lassen Peak, which spans from British Columbia in Canada to northern California in the United States. Volcanoes in the range have been produced by subduction of the Juan de Fuca tectonic plate under the North American Plate.

Geographic entities mentioned:
surface_form: Mount Garibaldi
instance_of: Mountain
countries: Canada
coordinates: lat: 49.850555555556
lon: -123.00472222222
surface_form: Lassen Peak
instance_of: Mountain
countries: United States
coordinates: lat: 40.488055555555555
lon: -121.505
surface_form: lassen peak
instance_of: Mountain
countries: United States
coordinates: lat: 40.488055555555555
lon: -121.505
Trout Creek Hill lies in the Quaternary Marble Mountain-Trout Creek Hill volcanic field in southern Washington state, formed by small basaltic and basaltic andesite shield volcanoes and cinder cones. This field runs from Marble Mountain to the area to the south of Trout Creek Hill. Located south of Mount St. Helens, it extends for and has a width of.

Geographic entities mentioned:
surface_form: Mount St. Helens
instance_of: Mountain
countries: United States
coordinates: lat: 46.200277777778
lon: -122.18944444444
surface_form: st. helens
instance_of: Mountain
countries: United States
coordinates: lat: 46.200277777778
lon: -122.18944444444
Trout Creek is a shield volcano. Small in size, it is topped by two nearby cinder cones that produced dark gray olivine basalt lava flows with glomeroporphyritic olivine inclusions. Hornblende andesite can also be found northwest of the Trout Creek Hill volcano, near West Crater. Eruptive history.

Geographic entities mentioned:
surface_form: West Crater
instance_of: Landform
countries: United States
coordinates: lat: 45.874
lon: -122.084
surface_form: west crater
instance_of: Landform
countries: United States
coordinates: lat: 45.874
lon: -122.084
surface_form: trout creek hill
instance_of: Mountain
countries: United States
coordinates: lat: 45.8365
lon: -121.995
surface_form: trout creek hill
instance_of: Mountain
countries: United States
coordinates: lat: 45.8365
lon: -121.995
Basaltic lavas from Trout Creek Hill show a lithology of pāhoehoe to blocky olivine, with pyroxene, breccia, scoria, and cinder deposits. Within the Marble Mountain–Trout Creek Hill field, there have been three eruptions during the Holocene epoch: at West Crater, another cone near Hackamore Creek, and a phreatic vent (producing steam and rock fragments) near Bare Mountain.

Geographic entities mentioned:
surface_form: bare mountain
instance_of: Mountain
countries: United States
coordinates: lat: 43.675277777778
lon: -75.073888888889
surface_form: west crater
instance_of: Landform
countries: United States
coordinates: lat: 45.874
lon: -122.084
surface_form: bare mountain
instance_of: Mountain
countries: United States
coordinates: lat: 42.3037
lon: -72.5314
surface_form: trout creek hill
instance_of: Mountain
countries: United States
coordinates: lat: 45.8365
lon: -121.995
These all took place about 8,000 years ago. The West Crater eruption generated an andesitic lava dome and lava flow, while the Bare Mountain vent formed a large explosion crater at Bare Mountain. Recreation.

Geographic entities mentioned:
surface_form: bare mountain
instance_of: Mountain
countries: United States
coordinates: lat: 43.675277777778
lon: -75.073888888889
surface_form: bare mountain
instance_of: Mountain
countries: United States
coordinates: lat: 43.675277777778
lon: -75.073888888889
surface_form: bare mountain
instance_of: Mountain
countries: United States
coordinates: lat: 42.3037
lon: -72.5314
surface_form: bare mountain
instance_of: Mountain
countries: United States
coordinates: lat: 42.3037
lon: -72.5314
The region has a &quot;rugged&quot; topography carved by glaciers and cirques, which have created glacial valleys. Trout Creek Hill and the rest of the Marble Mountain–Trout Creek Hill field can be accessed by roads in the Gifford Pinchot National Forest and Mount St. Helens National Volcanic Monument. Washington Route 503 and Forest Service Route 90 lie to the east of Woodland.

Geographic entities mentioned:
surface_form: mount st. helens national volcanic monument
instance_of: Mountain
countries: United States
coordinates: lat: 46.200277777778
lon: -122.18944444444
surface_form: st. helens
instance_of: Mountain
countries: United States
coordinates: lat: 46.200277777778
lon: -122.18944444444
surface_form: marble mountain
instance_of: Mountain
countries: United States
coordinates: lat: 58.64139
lon: -136.30333
surface_form: marble mountain
instance_of: Mountain
countries: United States
coordinates: lat: 40.7309
lon: -75.161
surface_form: trout creek hill
instance_of: Mountain
countries: United States
coordinates: lat: 45.8365
lon: -121.995
Moreover, there are only three significantly altered deposits along the Bear Creek. Trout Creek Hill lies in the Quaternary Marble Mountain-Trout Creek Hill volcanic field in southern Washington state, formed by small basaltic and basaltic andesite shield volcanoes and cinder cones. This field runs from Marble Mountain to the area to the south of Trout Creek Hill. Located south of Mount St.

Geographic entities mentioned:
surface_form: marble mountain
instance_of: Mountain
countries: United States
coordinates: lat: 58.64139
lon: -136.30333
surface_form: marble mountain
instance_of: Mountain
countries: United States
coordinates: lat: 40.7309
lon: -75.161
surface_form: trout creek hill
instance_of: Mountain
countries: United States
coordinates: lat: 45.8365
lon: -121.995
Trout Creek Hill. Trout Creek Hill is a small Pleistocene basaltic shield volcano in Washington, United States. Located in Skamania County, Trout Creek Hill rises to an elevation of. It is part of the Cascade Volcanic Arc, located in the Marble Mountain-Trout Creek Hill volcanic field.

Geographic entities mentioned:
surface_form: washington
instance_of: Lake
countries: United States
coordinates: lat: 47.616666666667
lon: -122.26472222222
surface_form: trout creek hill
instance_of: Mountain
countries: United States
coordinates: lat: 45.8365
lon: -121.995
A shield volcano, it has two cinder cones atop it. The nearby area is forested and hosts the Wind River Experimental Forest, and it can be hiked. Geography and access. Located in Skamania County in Washington state, in the United States, Trout Creek Hill rises to an elevation of. It is also known as Trout Hill, and was registered with the United States Geographic Names Information System in 1979.

Geographic entities mentioned:
surface_form: washington
instance_of: Lake
countries: United States
coordinates: lat: 47.616666666667
lon: -122.26472222222
surface_form: trout creek hill
instance_of: Mountain
countries: United States
coordinates: lat: 45.8365
lon: -121.995
Known as &quot;the cradle of forest research in the Pacific Northwest&quot;, the Wind River Forest represents a center for ecological research. It lies east of Vancouver, Washington, and it is administered by the United States Forest Service Pacific Northwest Research Station and the Gifford Pinchot National Forest.

Geographic entities mentioned:
surface_form: washington
instance_of: Lake
countries: United States
coordinates: lat: 47.616666666667
lon: -122.26472222222
Divided into the Ohanapecosh Formation, Eagle Creek Formation, Yakima Basalt, and Quaternary basalt flows, they show variable thickness and topographies. The Cascade Arc formed during the Oligocene epoch, and by the late Miocene epoch there was a low but broad gap between the Washington segment of the arc and Cascade volcanoes in Oregon.

Geographic entities mentioned:
surface_form: washington
instance_of: Lake
countries: United States
coordinates: lat: 47.616666666667
lon: -122.26472222222
The Cascade Arc formed during the Oligocene epoch, and by the late Miocene epoch there was a low but broad gap between the Washington segment of the arc and Cascade volcanoes in Oregon. Activity picked up during the Quaternary period in Washington, as andesitic stratovolcanoes and small, olivine basalt cinder cones and shield volcanoes erupted.

Geographic entities mentioned:
surface_form: washington
instance_of: Lake
countries: United States
coordinates: lat: 47.616666666667
lon: -122.26472222222
Moreover, there are only three significantly altered deposits along the Bear Creek. Trout Creek Hill lies in the Quaternary Marble Mountain-Trout Creek Hill volcanic field in southern Washington state, formed by small basaltic and basaltic andesite shield volcanoes and cinder cones. This field runs from Marble Mountain to the area to the south of Trout Creek Hill. Located south of Mount St.

Geographic entities mentioned:
surface_form: washington
instance_of: Lake
countries: United States
coordinates: lat: 47.616666666667
lon: -122.26472222222
surface_form: marble mountain
instance_of: Mountain
countries: United States
coordinates: lat: 58.64139
lon: -136.30333
surface_form: marble mountain
instance_of: Mountain
countries: United States
coordinates: lat: 40.7309
lon: -75.161
surface_form: trout creek hill
instance_of: Mountain
countries: United States
coordinates: lat: 45.8365
lon: -121.995
This eruption produced high-alumina olivine basalt, which make up the shield volcano and possess a dark gray color. Lava flows from the two cinder cones on Trout Creek Hill did not move far to the west from their source vents, instead moving to the southeast down the Wind River Valley into the Columbia River and around Bunker Hill.

Geographic entities mentioned:
surface_form: bunker hill
instance_of: Mountain
countries: United States
coordinates: lat: 39.2529
lon: -117.126
surface_form: bunker hill
instance_of: Mountain
countries: United States
coordinates: lat: 42.376361111111
lon: -71.060777777778
surface_form: trout creek hill
instance_of: Mountain
countries: United States
coordinates: lat: 45.8365
lon: -121.995
surface_form: river valley
instance_of: Valley
countries: United States
coordinates: lat: 35.36
lon: -93.37
surface_form: river valley
instance_of: Valley
countries: United States
coordinates: lat: 35.36
lon: -93.37
Ecology. The area around Trout Creek Hill contains the Wind River Experimental Forest, which contains Western hemlock, Douglas fir, and Pacific silver fir. Known as &quot;the cradle of forest research in the Pacific Northwest&quot;, the Wind River Forest represents a center for ecological research.

Geographic entities mentioned:
surface_form: hemlock
instance_of: Lake
countries: United States
coordinates: lat: 42.718611111111
lon: -77.608888888889
surface_form: trout creek hill
instance_of: Mountain
countries: United States
coordinates: lat: 45.8365
lon: -121.995
However, the six or seven emplaced lava flow deposits in the area only show small amounts of alteration to the west of the valley, and they show no alteration to the east. Moreover, there are only three significantly altered deposits along the Bear Creek.

Geographic entities mentioned:
surface_form: bear creek
instance_of: Watercourse
countries: United States
coordinates: lat: 39.8305929
lon: -92.2301817
Within Wind River valley, these deposits reach depths of more than at the Bear Creek, Panther Creek, and Wind River junction; the shorter flows that extended to the west likely exceed thicknesses of with lengths of. Other lava flows from Trout Creek Hill are also embedded with till from Salmon Springs and Fraser Glaciation, but their exact age is unknown.

Geographic entities mentioned:
surface_form: bear creek
instance_of: Watercourse
countries: United States
coordinates: lat: 39.8305929
lon: -92.2301817