Sarmila/GeoWiki-Features huggingface dataset:
Topography. The parish of Kilcronaghan lies on the descending slope of Slieve Gallion (), with its highest point lying in the townland of Gortahurk, above sea level. From here it slopes downwards to low gravelly hills, which predominate in the parish. This series of hills become more broken and irregular as they approach the River Moyola.

Geographic entities mentioned:
surface_form: Slieve Gallion
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.73
lon: -6.76
Broadcasting career. Born in Sudbury, Ontario, Erola worked as a radio and television broadcaster in Sudbury. At CKSO-TV, she made history as the first woman employed by a Canadian television station as a weather reporter, and also presented segments on fashion. She later became an account executive for CHNO, and married Voito (Vic) Erola, the owner of a marina on Lake Panache, in 1955. Politics.

Geographic entities mentioned:
surface_form: Lake Panache
instance_of: Lake
countries: Canada
coordinates: lat: 46.25
lon: -81.3167
Future eruptions are likely to impact local streams and cause wildfires. Several streams surround the MEVC, many of which drain the flanks of the volcanic complex. They include the Little Iskut River along the southeastern flank, Kakiddi Creek along the northeastern flank, the Klastline River along the northern flank and Mess Creek along the western flank.

Geographic entities mentioned:
surface_form: Little Iskut River
instance_of: Watercourse
countries: Canada
coordinates: lat: 57.448889
lon: -130.268611
surface_form: Kakiddi Creek
instance_of: Watercourse
countries: Canada
coordinates: lat: 57.872778
lon: -130.425556
surface_form: Mess Creek
instance_of: Watercourse
countries: Canada
coordinates: lat: 57.88296
lon: -131.2206
A number of explanations have been made regarding the origin of the name Edziza. A 1927 report by J. Davidson of the British Columbia Land Surveyors claims that Edziza means &quot;sand&quot; in the Tahltan language, referring to the deep volcanic ash deposits or pumice-like sand covering large portions of the Big Raven Plateau around Mount Edziza.

Geographic entities mentioned:
surface_form: Big Raven Plateau
instance_of: Plateau
countries: Canada
coordinates: lat: 57.7167
lon: -130.75
surface_form: Mount Edziza
instance_of: Mountain
countries: Canada
coordinates: lat: 57.715555555555554
lon: -130.63472222222222
surface_form: columbia
instance_of: Mountain
countries: Canada
coordinates: lat: 52.1475
lon: -117.44055555555556
Its sides tower above adjacent valleys that serve as drainageways for several streams. The edges of the plateau have been deeply incised by creeks that flow eastward and westward into Mess Creek, Kakiddi Creek and the Iskut River. A northerly-trending, elliptical, composite shield volcano consisting of multiple flat-lying lava flows forms the plateau. Location.

Geographic entities mentioned:
surface_form: Mess Creek
instance_of: Watercourse
countries: Canada
coordinates: lat: 57.88296
lon: -131.2206
surface_form: Kakiddi Creek
instance_of: Watercourse
countries: Canada
coordinates: lat: 57.872778
lon: -130.425556
surface_form: mess creek
instance_of: Watercourse
countries: Canada
coordinates: lat: 57.88296
lon: -131.2206
Location. The MEVC is surrounded on the east by the Skeena Mountains and the Klastline Plateau whereas to the west it is flanked by the Coast Mountains. It lies on the eastern edge of the Tahltan Highland, a southeast-trending upland area extending along the western side of the Stikine Plateau between the Boundary Ranges in the west and the head of the Iskut River in the east.

Geographic entities mentioned:
surface_form: Klastline Plateau
instance_of: Plateau
countries: Canada
coordinates: lat: 57.95
lon: -130.083
Location. The MEVC is surrounded on the east by the Skeena Mountains and the Klastline Plateau whereas to the west it is flanked by the Coast Mountains. It lies on the eastern edge of the Tahltan Highland, a southeast-trending upland area extending along the western side of the Stikine Plateau between the Boundary Ranges in the west and the head of the Iskut River in the east.

Geographic entities mentioned:
surface_form: Stikine Plateau
instance_of: Plateau
countries: Canada
coordinates: lat: 58.38305555555556
lon: -129.885
It is a large ice-covered stratovolcano rising well above the general level of the Tahltan Highland. Ice Peak is a composite stratovolcano in elevation that has been reduced to a steep-walled pyramidal peak with active cirques on all of its sides. The Spectrum Range has an elevation of and consists of a nearly circular, more than wide dome with a thickness of up to.

Geographic entities mentioned:
surface_form: Ice Peak
instance_of: Mountain
countries: Canada
coordinates: lat: 57.6906
lon: -130.635
The Spectrum Range has an elevation of and consists of a nearly circular, more than wide dome with a thickness of up to. Armadillo Peak represents the eroded remains of a small caldera whose summit is capped by a thick sequence of ponded lava flows. Various stages of erosion have modified these central volcanoes; in some cases, only a few small remnants of their original surface remain.

Geographic entities mentioned:
surface_form: Armadillo Peak
instance_of: Mountain
countries: Canada
coordinates: lat: 57.5383
lon: -130.56
Several cinder cones dotting the plateau surface rise up to above the surrounding terrain, most of which occur in three lava fields. The Desolation Lava Field on the northern slope of Mount Edziza contains 10 cinder cones, namely Eve Cone, Storm Cone, Moraine Cone, Williams Cone, Sleet Cone, Twin Cone, Sidas Cone and the three Triplex Cones.

Geographic entities mentioned:
surface_form: Eve Cone
instance_of: Mountain
countries: Canada
coordinates: lat: 57.81305555555556
lon: -130.67555555555555
surface_form: Williams Cone
instance_of: Mountain
countries: Canada
coordinates: lat: 57.78
lon: -130.599
surface_form: Sidas Cone
instance_of: Mountain
countries: Canada
coordinates: lat: 57.8589
lon: -130.628
surface_form: eve cone
instance_of: Mountain
countries: Canada
coordinates: lat: 57.81305555555556
lon: -130.67555555555555
The Desolation Lava Field on the northern slope of Mount Edziza contains 10 cinder cones, namely Eve Cone, Storm Cone, Moraine Cone, Williams Cone, Sleet Cone, Twin Cone, Sidas Cone and the three Triplex Cones. Five named cones occur in the Snowshoe Lava Field on the southwestern flank of Ice Peak: Tennena Cone, Keda Cone, Coffee Crater, Cocoa Crater and The Saucer.

Geographic entities mentioned:
surface_form: Tennena Cone
instance_of: Mountain
countries: Canada
coordinates: lat: 57.68416666666667
lon: -130.66222222222223
surface_form: Coffee Crater
instance_of: Mountain
countries: Canada
coordinates: lat: 57.63
lon: -130.67
surface_form: Cocoa Crater
instance_of: Mountain
countries: Canada
coordinates: lat: 57.65
lon: -130.7
Five named cones occur in the Snowshoe Lava Field on the southwestern flank of Ice Peak: Tennena Cone, Keda Cone, Coffee Crater, Cocoa Crater and The Saucer. The Ash Pit is the only named cinder cone in the Mess Lake Lava Field which lies at the south-central end of the MEVC.

Geographic entities mentioned:
surface_form: The Ash Pit
instance_of: Mountain
countries: Canada
coordinates: lat: 57.45
lon: -130.78
The Ash Pit is the only named cinder cone in the Mess Lake Lava Field which lies at the south-central end of the MEVC. Isolated cinder cones include Icefall Cone and Ridge Cone on the eastern slope of Mount Edziza, Nahta Cone at the extreme southern end of the MEVC, Kana Cone on the extreme northern flank of the MEVC and two unnamed cones in Walkout Creek valley.

Geographic entities mentioned:
surface_form: Nahta Cone
instance_of: Mountain
countries: Canada
coordinates: lat: 57.3083
lon: -130.821
Two lava fields are present on the Big Raven Plateau; the Desolation Lava Field at the northern end of the plateau covers more than whereas the Snowshoe Lava Field covers about at the southern end of the plateau. At the northwestern end of the Spectrum Range is the Kitsu Plateau; its dominant feature is the even smaller Mess Lake Lava Field which covers.

Geographic entities mentioned:
surface_form: Kitsu Plateau
instance_of: Plateau
countries: Canada
coordinates: lat: 57.4667
lon: -130.75
surface_form: kitsu plateau
instance_of: Plateau
countries: Canada
coordinates: lat: 57.4667
lon: -130.75
At the northwestern end of the Spectrum Range is the Kitsu Plateau; its dominant feature is the even smaller Mess Lake Lava Field which covers. The Arctic Lake Plateau is the southernmost of the three subplateaus; it consists of a nearly flat upland containing Outcast Hill, Tadekho Hill, Wetalth Ridge, Nahta Cone, Source Hill, Thaw Hill and Exile Hill.

Geographic entities mentioned:
surface_form: Arctic Lake Plateau
instance_of: Plateau
countries: Canada
coordinates: lat: 57.3
lon: -130.767
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: 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
surface_form: outcast hill
instance_of: Mountain
countries: Canada
coordinates: lat: 57.39
lon: -130.774
The Arctic Lake Plateau is the southernmost of the three subplateaus; it consists of a nearly flat upland containing Outcast Hill, Tadekho Hill, Wetalth Ridge, Nahta Cone, Source Hill, Thaw Hill and Exile Hill. In the north fork of Tenchen Creek is Cinder Cliff, a high barrier of volcanic rocks. Koosick Bluff and Ornostay Bluff are just southwest of Mount Edziza near the head of Sezill Creek.

Geographic entities mentioned:
surface_form: Tenchen Creek
instance_of: Watercourse
countries: Canada
coordinates: lat: 57.76636
lon: -130.43724
In the north fork of Tenchen Creek is Cinder Cliff, a high barrier of volcanic rocks. Koosick Bluff and Ornostay Bluff are just southwest of Mount Edziza near the head of Sezill Creek. Northwest and east of Coffee Crater are Hoia Bluff and Kaia Bluff, respectively. Hoia Bluff is a prominent west-facing cliff whereas Kaia Bluff is a steep-sided hill.

Geographic entities mentioned:
surface_form: Koosick Bluff
instance_of: Mountain
countries: Canada
coordinates: lat: 57.6739
lon: -130.725
surface_form: Ornostay Bluff
instance_of: Mountain
countries: Canada
coordinates: lat: 57.699722222222
lon: -130.70388888889
surface_form: Sezill Creek
instance_of: Watercourse
countries: Canada
coordinates: lat: 57.69967
lon: -130.88724
It runs along the eastern side of Mess Creek and exposes thick, flat-lying lava flows. Artifact Ridge is a crescent-shaped mountain ridge east of the Kitsu Plateau and just north of Artifact Creek. Just south of Artifact Ridge and Artifact Creek is Obsidian Ridge, a mountain ridge containing high-quality obsidian.

Geographic entities mentioned:
surface_form: Artifact Creek
instance_of: Watercourse
countries: Canada
coordinates: lat: 57.41635
lon: -130.53728
surface_form: kitsu plateau
instance_of: Plateau
countries: Canada
coordinates: lat: 57.4667
lon: -130.75
Destell Pass is a narrow rock cleft northwest of Artifact Ridge that provides access between the broad upland valleys of Artifact Creek and Raspberry Creek. It is one of two named mountain passes in the MEVC, the other being Raspberry Pass between the heads of Bourgeaux Creek and Raspberry Creek.

Geographic entities mentioned:
surface_form: Bourgeaux Creek
instance_of: Watercourse
countries: Canada
coordinates: lat: 57.49966
lon: -130.45397
Lakes. The eastern side of the MEVC is flanked by Mowdade Lake, Kakiddi Lake, Mowchilla Lake and Nuttlude Lake in Kakiddi Valley; the last three drain north into the Klastline River. Buckley Lake is the main lake bordering the northern side of the MEVC whereas Mess Lake is the main lake bordering the western side of the MEVC.

Geographic entities mentioned:
surface_form: Mess Lake
instance_of: Lake
countries: Canada
coordinates: lat: 57.4667
lon: -130.883
Two small lakes are named on the southern portion of the MEVC. At the head of the Little Iskut River is Little Ball Lake, also called Kounugu Lake after the guardian of fresh water in Tahltan folklore. It lies immediately south of Kounugu Mountain in the Spectrum Range and east of Ball Creek. Little Arctic Lake lies northeast of Arctic Lake near the northeastern flank of Wetalth Ridge. Drainage.

Geographic entities mentioned:
surface_form: Little Iskut River
instance_of: Watercourse
countries: Canada
coordinates: lat: 57.448889
lon: -130.268611
surface_form: Little Ball Lake
instance_of: Lake
countries: Canada
coordinates: lat: 57.34889
lon: -130.58917
Two small lakes are named on the southern portion of the MEVC. At the head of the Little Iskut River is Little Ball Lake, also called Kounugu Lake after the guardian of fresh water in Tahltan folklore. It lies immediately south of Kounugu Mountain in the Spectrum Range and east of Ball Creek. Little Arctic Lake lies northeast of Arctic Lake near the northeastern flank of Wetalth Ridge. Drainage.

Geographic entities mentioned:
surface_form: Kounugu Mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 57.3647
lon: -130.5973
surface_form: ball creek
instance_of: Watercourse
countries: Canada
coordinates: lat: 58.38284
lon: -129.18684
This includes Crayke Creek which flows to the southwest, Elwyn Creek which flows to the west, Kitsu Creek which flows to the northwest, Raspberry Creek which flows to the northwest, Tadekho Creek which flows to the northwest and Taweh Creek which flows to the northwest.

Geographic entities mentioned:
surface_form: Crayke Creek
instance_of: Watercourse
countries: Canada
coordinates: lat: 57.73298
lon: -130.97063
surface_form: Elwyn Creek
instance_of: Watercourse
countries: Canada
coordinates: lat: 57.78298
lon: -130.98722
surface_form: Kitsu Creek
instance_of: Watercourse
countries: Canada
coordinates: lat: 57.51636
lon: -130.85398
surface_form: Tadekho Creek
instance_of: Watercourse
countries: Canada
coordinates: lat: 57.43296
lon: -130.90399
surface_form: Taweh Creek
instance_of: Watercourse
countries: Canada
coordinates: lat: 57.71638
lon: -130.97063
surface_form: kitsu creek
instance_of: Watercourse
countries: Canada
coordinates: lat: 57.51636
lon: -130.85398
surface_form: taweh creek
instance_of: Watercourse
countries: Canada
coordinates: lat: 57.71638
lon: -130.97063
Many of these Mess Creek tributaries also contain tributaries; the only named tributary of Elwyn Creek is Kadeya Creek which flows northwest from Mount Edziza. Kitsu Creek contains one named tributary, Nagha Creek, which flows northwest from the Spectrum Range.

Geographic entities mentioned:
surface_form: Kadeya Creek
instance_of: Watercourse
countries: Canada
coordinates: lat: 57.79967
lon: -130.87063
surface_form: Mount Edziza
instance_of: Mountain
countries: Canada
coordinates: lat: 57.715555555555554
lon: -130.63472222222222
Kitsu Creek contains one named tributary, Nagha Creek, which flows northwest from the Spectrum Range. Walkout Creek is the only named tributary of Raspberry Creek; it flows west in a canyon west of the Armadillo Highlands and also contains only one named tributary, Flyin Creek, which flows northwest from near the west side of Cache Hill.

Geographic entities mentioned:
surface_form: Flyin Creek
instance_of: Watercourse
countries: Canada
coordinates: lat: 57.56636
lon: -130.75397
Its upper eastern half is drained by tributaries of Kakiddi Creek. This includes Nido Creek, Tenchen Creek and Tennaya Creek which flow to the northeast from the eastern side of Mount Edziza, Shaman Creek and Sorcery Creek which flow to the east and north from near Kaia Bluff and Tsecha Creek which flows to the northeast from near Williams Cone.

Geographic entities mentioned:
surface_form: Nido Creek
instance_of: Watercourse
countries: Canada
coordinates: lat: 57.71636
lon: -130.47065
surface_form: Tennaya Creek
instance_of: Watercourse
countries: Canada
coordinates: lat: 57.69966
lon: -130.42065
surface_form: Shaman Creek
instance_of: Watercourse
countries: Canada
coordinates: lat: 57.61636
lon: -130.40395
surface_form: Tsecha Creek
instance_of: Watercourse
countries: Canada
coordinates: lat: 57.83296
lon: -130.42064
surface_form: tsecha creek
instance_of: Watercourse
countries: Canada
coordinates: lat: 57.83296
lon: -130.42064
This includes Nido Creek, Tenchen Creek and Tennaya Creek which flow to the northeast from the eastern side of Mount Edziza, Shaman Creek and Sorcery Creek which flow to the east and north from near Kaia Bluff and Tsecha Creek which flows to the northeast from near Williams Cone. Shaman Creek contains one named tributary, Chakima Creek, which flows to the east and north.

Geographic entities mentioned:
surface_form: Chakima Creek
instance_of: Watercourse
countries: Canada
coordinates: lat: 57.59966
lon: -130.42066
The lower eastern half and south end of the MEVC are drained by tributaries of the Iskut River. This includes Ball Creek which flows to the south from the southeastern side of the Spectrum Range, More Creek which flows to the southeast from the southern side of the Spectrum Range and the Little Iskut River which flows to the southeast from the southeastern side of the Spectrum Range.

Geographic entities mentioned:
surface_form: More Creek
instance_of: Watercourse
countries: Canada
coordinates: lat: 57.03294
lon: -130.35401
surface_form: ball creek
instance_of: Watercourse
countries: Canada
coordinates: lat: 58.38284
lon: -129.18684
The only named tributary of Ball Creek is Chachani Creek which flows to the southeast from the eastern end of the Arctic Lake Plateau. Tributaries of the Little Iskut River include Stewbomb Creek, which flows eastwards from the eastern side of the Spectrum Range, and Bourgeaux Creek which flows to the east from Raspberry Pass.

Geographic entities mentioned:
surface_form: Stewbomb Creek
instance_of: Watercourse
countries: Canada
coordinates: lat: 57.41635
lon: -130.50397
The only named tributary of Stewbomb Creek is Artifact Creek which flows to the southeast between Artifact Ridge and Obsidian Ridge. Bourgeaux Creek contains one named tributary, Gerlib Creek, which flows southwards from between Tadeda Peak and Armadillo Peak. Several small, unnamed streams drain the youthful northern side of the MEVC.

Geographic entities mentioned:
surface_form: Tadeda Peak
instance_of: Mountain
countries: Canada
coordinates: lat: 57.5422
lon: -130.616
surface_form: armadillo peak
instance_of: Mountain
countries: Canada
coordinates: lat: 57.5383
lon: -130.56
South of Mount Edziza lies Tencho Glacier, the largest glacier of the MEVC. Tennaya Glacier lies at the head of Tennaya Creek on the southeastern side of Mount Edziza. The informally named Yeda Glacier existed at the head of Ball Creek south of Yeda Peak in the Spectrum Range in 1988. Background.

Geographic entities mentioned:
surface_form: Yeda Peak
instance_of: Mountain
countries: Canada
coordinates: lat: 57.3811
lon: -130.678
surface_form: ball creek
instance_of: Watercourse
countries: Canada
coordinates: lat: 58.38284
lon: -129.18684
The informally named Yeda Glacier existed at the head of Ball Creek south of Yeda Peak in the Spectrum Range in 1988. Background. The MEVC is part of the Northern Cordilleran Volcanic Province (NCVP), a broad area of shield volcanoes, lava domes, cinder cones and stratovolcanoes extending 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
The MEVC is part of a subdivision of the NCVP called the Stikine Subprovince. This subprovince, confined to the Stikine region of northwestern British Columbia, includes three other volcanic complexes: Heart Peaks, Hoodoo Mountain and Level Mountain. The four complexes differ petrologically and/or volumetrically from the rest of the NCVP.

Geographic entities mentioned:
surface_form: Heart Peaks
instance_of: Mountain
countries: Canada
coordinates: lat: 58.5989
lon: -131.963
surface_form: Hoodoo Mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 56.772222222222
lon: -131.29444444444
surface_form: columbia
instance_of: Mountain
countries: Canada
coordinates: lat: 52.1475
lon: -117.44055555555556
Souther began detailed mapping of the MEVC in 1965 when he was given the job of working on the volcanic complex by the Geological Survey of Canada. Japanese volcanologist Hisashi Kuno visited the MEVC with Souther in 1966; Kuno Peak in the Spectrum Range was named in his honour.

Geographic entities mentioned:
surface_form: Kuno Peak
instance_of: Mountain
countries: Canada
coordinates: lat: 57.3763
lon: -130.7398
A hiking trail dubbed the Buckley Lake to Mowdade Lake Route extends across the northern half of the MEVC. It traverses south from Buckley Lake along Buckley Creek and gradually climbs onto the MEVC plateau where Eve Cone, Sidas Cone and Tsekone Ridge are visible along the route. Most of the Buckley Lake to Mowdade Lake Route is marked by a series of rock cairns from Tsekone Ridge onwards.

Geographic entities mentioned:
surface_form: Tsekone Ridge
instance_of: Mountain
countries: Canada
coordinates: lat: 57.77
lon: -130.69
surface_form: eve cone
instance_of: Mountain
countries: Canada
coordinates: lat: 57.81305555555556
lon: -130.67555555555555
surface_form: buckley lake
instance_of: Lake
countries: Canada
coordinates: lat: 57.905833
lon: -130.778056
Hoia Bluff is a prominent west-facing cliff whereas Kaia Bluff is a steep-sided hill. On the northwestern side of Raspberry Pass is an isolated, flat-topped hill with steep sides called Gnu Butte. The Mess Creek Escarpment is a long, often cliff-like feature forming the western edge of the MEVC. It runs along the eastern side of Mess Creek and exposes thick, flat-lying lava flows.

Geographic entities mentioned:
surface_form: mess creek
instance_of: Watercourse
countries: Canada
coordinates: lat: 57.88296
lon: -131.2206
Evidence of ice stagnation is present in the form of outflow channels, eskers, kames, kettles and morainal ridges on the northern side of the MEVC adjacent to Buckley Lake. Deglaciation of unstable and oversteepened valley walls has caused several landslides in the geologic past, especially along the Mess Creek Escarpment.

Geographic entities mentioned:
surface_form: mess creek
instance_of: Watercourse
countries: Canada
coordinates: lat: 57.88296
lon: -131.2206
The downthrowing of this fault during the Holocene may have been due to the draining of magma chambers following eruptions at the MEVC. The existence of peralkaline rocks at the MEVC and the presence of normal faults along Mess Creek valley support the conclusion that the MEVC lies in an area of continental rifting.

Geographic entities mentioned:
surface_form: mess creek
instance_of: Watercourse
countries: Canada
coordinates: lat: 57.88296
lon: -131.2206
Hydrothermal activity. The MEVC is volcanically dormant but it still remains hydrothermally active. Four hot spring areas are found along the western flank of the MEVC at Mess Lake, Mess Creek, Elwyn Creek and Sezill Creek, the latter three of which have recorded water temperatures of, and, respectively.

Geographic entities mentioned:
surface_form: mess creek
instance_of: Watercourse
countries: Canada
coordinates: lat: 57.88296
lon: -131.2206
Discharge at the Sezill Creek, Elwyn Creek and Mess Lake hot springs may be linked to shallow hydrothermal systems driven by residual magmatic heat as they are adjacent to recently active eruptive centres. In contrast, the Mess Creek Hot Springs may be discharging from a deeply circulating hydraulic system along a major fault on the western side of Mess Creek valley.

Geographic entities mentioned:
surface_form: mess creek
instance_of: Watercourse
countries: Canada
coordinates: lat: 57.88296
lon: -131.2206
These springs had a vigorous flow of warm water in 1965, but by 1992 they were discharging water below human body temperature. The Mess Creek Hot Springs south of Mess Lake are on the western side of Mess Creek where they attain an elevation of. Along the banks of Elwyn Creek at an elevation of are the Elwyn Hot Springs which have created thick tufa deposits.

Geographic entities mentioned:
surface_form: mess creek
instance_of: Watercourse
countries: Canada
coordinates: lat: 57.88296
lon: -131.2206
Extending from these roads are horse trails that provide access to the MEVC. From Telegraph Creek, the Buckley Lake Trail extends about southeast along Mess Creek and Three Mile Lake. It then traverses about northeast along Dagaichess Creek and Stinking Lake to the northeastern end of Buckley Lake where it meets with the Klastline River Trail and the Buckley Lake to Mowdade Lake Route.

Geographic entities mentioned:
surface_form: mess creek
instance_of: Watercourse
countries: Canada
coordinates: lat: 57.88296
lon: -131.2206
From there, it enters Mount Edziza Provincial Park and continues another west along Bourgeaux Creek into the central portion of the MEVC at Raspberry Pass. The Yukon Telegraph Trail then traverses about northwest along Raspberry Creek into the broad valley of Mess Creek where it continues another north along the western side of the MEVC. It conjoins with the Buckley Lake Trail near Matheson Creek.

Geographic entities mentioned:
surface_form: mess creek
instance_of: Watercourse
countries: Canada
coordinates: lat: 57.88296
lon: -131.2206
Evidence of ice stagnation is present in the form of outflow channels, eskers, kames, kettles and morainal ridges on the northern side of the MEVC adjacent to Buckley Lake. Deglaciation of unstable and oversteepened valley walls has caused several landslides in the geologic past, especially along the Mess Creek Escarpment.

Geographic entities mentioned:
surface_form: buckley lake
instance_of: Lake
countries: Canada
coordinates: lat: 57.905833
lon: -130.778056
About 20 microearthquakes potentially associated with the MEVC were recorded by seismographs installed at Buckley Lake and Nuttlude Lake, but a seismological analysis suggested that they were of non-volcanic origin. The microearthquakes had magnitudes of around 0.5 which typically occur in many areas throughout the Canadian Cordillera.

Geographic entities mentioned:
surface_form: buckley lake
instance_of: Lake
countries: Canada
coordinates: lat: 57.905833
lon: -130.778056
Horseback riding at the MEVC requires a letter of authorization. The many cinder cones dotting the MEVC have designated climbing routes to prevent scarring on their delicate surfaces from foot traffic. A hiking trail dubbed the Buckley Lake to Mowdade Lake Route extends across the northern half of the MEVC.

Geographic entities mentioned:
surface_form: buckley lake
instance_of: Lake
countries: Canada
coordinates: lat: 57.905833
lon: -130.778056
A hiking trail dubbed the Buckley Lake to Mowdade Lake Route extends across the northern half of the MEVC. It traverses south from Buckley Lake along Buckley Creek and gradually climbs onto the MEVC plateau where Eve Cone, Sidas Cone and Tsekone Ridge are visible along the route. Most of the Buckley Lake to Mowdade Lake Route is marked by a series of rock cairns from Tsekone Ridge onwards.

Geographic entities mentioned:
surface_form: buckley lake
instance_of: Lake
countries: Canada
coordinates: lat: 57.905833
lon: -130.778056
Most of the Buckley Lake to Mowdade Lake Route is marked by a series of rock cairns from Tsekone Ridge onwards. The distance between Buckley Lake and Mowdade Lake is about but the hiking length between these two lakes varies depending on the route taken; it can take a minimum of 7 days to hike the Buckley Lake to Mowdade Lake Route. The weather can change extremely fast along this hiking trail.

Geographic entities mentioned:
surface_form: buckley lake
instance_of: Lake
countries: Canada
coordinates: lat: 57.905833
lon: -130.778056
Extending from these roads are horse trails that provide access to the MEVC. From Telegraph Creek, the Buckley Lake Trail extends about southeast along Mess Creek and Three Mile Lake. It then traverses about northeast along Dagaichess Creek and Stinking Lake to the northeastern end of Buckley Lake where it meets with the Klastline River Trail and the Buckley Lake to Mowdade Lake Route.

Geographic entities mentioned:
surface_form: buckley lake
instance_of: Lake
countries: Canada
coordinates: lat: 57.905833
lon: -130.778056
surface_form: buckley lake
instance_of: Lake
countries: Canada
coordinates: lat: 57.905833
lon: -130.778056
After entering Mount Edziza Provincial Park, the Klastline River Trail traverses northwest along the Klastline River for about and then crosses the river north of the MEVC. From there, the Klastline River Trail traverses west for about to the northeastern end of Buckley Lake where it meets with the Buckley Lake Trail and Buckley Lake to Mowdade Lake Route.

Geographic entities mentioned:
surface_form: buckley lake
instance_of: Lake
countries: Canada
coordinates: lat: 57.905833
lon: -130.778056
surface_form: buckley lake
instance_of: Lake
countries: Canada
coordinates: lat: 57.905833
lon: -130.778056
surface_form: buckley lake
instance_of: Lake
countries: Canada
coordinates: lat: 57.905833
lon: -130.778056
Private aircraft are prohibited from landing on the Kitsu Plateau lava flows. Kakiddi Lake, 180 Lake, Mess Lake, Arctic Lake, Nuttlude Lake, Mowdade Lake, Little Arctic Lake, Little Ball Lake, Mowchilla Lake and Buckley Lake are large enough to be used by float-equipped aircraft.

Geographic entities mentioned:
surface_form: buckley lake
instance_of: Lake
countries: Canada
coordinates: lat: 57.905833
lon: -130.778056
surface_form: ball lake
instance_of: Lake
countries: Canada
coordinates: lat: 49.7
lon: -125.317
Mount Edziza volcanic complex. The Mount Edziza volcanic complex (; abbreviated MEVC) is a group of volcanoes and associated lava flows in northwestern British Columbia, Canada. Located on the Tahltan Highland, it is southeast of Telegraph Creek and southwest of Dease Lake. The complex encompasses a broad, steep-sided lava plateau that extends over.

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
The MEVC is in the Southern Boreal Plateau Ecosection which consists of several upland summits as well as wide river valleys and deeply incised plateaus. It is one of seven ecosections comprising the Boreal Mountains and Plateaus Ecoregion, a large ecological region of northwestern British Columbia encompassing high plateaus and rugged mountains with intervening lowlands.

Geographic entities mentioned:
surface_form: columbia
instance_of: Mountain
countries: Canada
coordinates: lat: 52.1475
lon: -117.44055555555556
The eruption sequence and style of the MEVC, along with its chemistry, mineralogy and isotopic composition, is similar to continental peralkaline volcanism at the Rainbow Range of central British Columbia, the Afar Depression of East Africa and parts of the Great Basin of the western United States.

Geographic entities mentioned:
surface_form: columbia
instance_of: Mountain
countries: Canada
coordinates: lat: 52.1475
lon: -117.44055555555556
Hazards and monitoring. Natural Resources Canada considers the MEVC a high threat volcanic complex because it has had the highest eruption rate in Canada throughout the Holocene. However, its extremely remote location makes it less hazardous than volcanoes in southwestern British Columbia.

Geographic entities mentioned:
surface_form: columbia
instance_of: Mountain
countries: Canada
coordinates: lat: 52.1475
lon: -117.44055555555556
Ash columns can drift for thousands of kilometres downwind and often become increasingly spread out over a larger area with increasing distance from an erupting vent. The MEVC lies under a major air route from Vancouver, British Columbia to Whitehorse, Yukon, suggesting the volcanic complex poses a potential threat to air traffic.

Geographic entities mentioned:
surface_form: columbia
instance_of: Mountain
countries: Canada
coordinates: lat: 52.1475
lon: -117.44055555555556
This volcanic glass was used in the manufacturing of projectile points and cutting blades which were widely traded throughout the Pacific Northwest. Obsidian from the MEVC has been recovered from archaeological sites in Alaska, Yukon, western Alberta and along the British Columbia Coast, making Edziza obsidian the most widely distributed obsidian in western North America.

Geographic entities mentioned:
surface_form: columbia
instance_of: Mountain
countries: Canada
coordinates: lat: 52.1475
lon: -117.44055555555556
Along the western side of the MEVC and through its central portion at Raspberry Pass are the remains of the Yukon Telegraph Line. This was a nearly long telegraphy system built by the Dominion Government Telegraph Service between 1897 and 1901 to send messages between Ashcroft, British Columbia in the south to Dawson City, Yukon in the north.

Geographic entities mentioned:
surface_form: columbia
instance_of: Mountain
countries: Canada
coordinates: lat: 52.1475
lon: -117.44055555555556
Yagi Ridge in the Spectrum Range was named in honour of Kenzō Yagi who traversed this ridge with Souther during their geological studies. During his last year of serious field work in 1992, Souther published an extensive bulletin on his work entitled &quot;The Late Cenozoic Mount Edziza Volcanic Complex, British Columbia&quot; which highlighted the importance and size of the MEVC.

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
In 1989, Mount Edziza Provincial Park roughly doubled in size when was annexed from the Mount Edziza Recreation Area. With this annexation, the recreation area was greatly reduced in size to around; it was eventually disestablished in 2003. Mount Edziza Provincial Park now covers an area of, making it 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
Most peaks greater than in elevation have glaciers. Small separate glaciers are largely restricted to the southern half of the MEVC where they occur in the Spectrum Range, on Armadillo Peak and elsewhere. In contrast, Mount Edziza and Ice Peak are obscured by a relatively large ice cap that covers an area of.

Geographic entities mentioned:
surface_form: armadillo peak
instance_of: Mountain
countries: Canada
coordinates: lat: 57.5383
lon: -130.56
Mount Edziza volcanic complex. The Mount Edziza volcanic complex (; abbreviated MEVC) is a group of volcanoes and associated lava flows in northwestern British Columbia, Canada. Located on the Tahltan Highland, it is southeast of Telegraph Creek and southwest of Dease Lake. The complex encompasses a broad, steep-sided lava plateau that extends over.

Geographic entities mentioned:
surface_form: mount edziza volcanic complex
instance_of: Mountain
countries: Canada
coordinates: lat: 57.5
lon: -130.6
A large provincial park, which can only be accessed by aircraft or by a network of horse trails, dominates the MEVC. Names and etymology. The Mount Edziza volcanic complex is sometimes referred to as the Mount Edziza–Spectrum Range complex or the Mount Edziza Plateau. Stratigraphically, it has also been referred to as the Mount Edziza Group or the Edziza Group.

Geographic entities mentioned:
surface_form: mount edziza volcanic complex
instance_of: Mountain
countries: Canada
coordinates: lat: 57.5
lon: -130.6
Despite this defeat, Nobunaga was inspired to launch another siege, the Siege of Mount Hiei. Siege of Mount Hiei. The Enryaku-ji temple on Mount Hiei was an issue for Nobunaga. The monastery's (warrior monks) of the Tendai school were aiding his opponents in the Azai-Asakura alliance and the temple was close to his base of power.

Geographic entities mentioned:
surface_form: Mount Hiei
instance_of: Mountain
countries: Japan
coordinates: lat: 35.066666666667
lon: 135.83833333333
Lahuachaca. Lahuachaca is a small town in Bolivia, in Aroma Province. It lies 123 km from La Paz, on the Bolivian Altiplano, with the Cordillera Occidental to the west and the Cordillera Central to the east. Climate. The average temperature in Lahuachaca is 9 °C. The average temperature varies from 7° in July to 11° in December. The average annual rainfall is 600 mm.

Geographic entities mentioned:
surface_form: Altiplano
instance_of: Plateau
countries: Bolivia
Peru
Chile
Argentina
coordinates: lat: -16.00358
lon: -69.65332
Pampa Wasi. Pampa Wasi (Quechua &quot;pampa&quot; a large plain, &quot;wasi&quot; house, &quot;plain house&quot;, also spelled &quot;Pampahuasi&quot;) is a mountain in the Andes of Peru. It is located in the Huánuco Region, Dos de Mayo Province, Marías District.

Geographic entities mentioned:
surface_form: pampa wasi
instance_of: Mountain
countries: Peru
coordinates: lat: -9.64305556
lon: -76.42111111
In 2009, SGI received funding from ExxonMobil to produce biofuels on an industrial-scale using recombinant algae and other microorganisms. The company purchased an in the Imperial Valley in Southern California to produce algae fuel for their collaboration with Exxon Mobil.

Geographic entities mentioned:
surface_form: Imperial Valley
instance_of: Valley
countries: United States
coordinates: lat: 33.1
lon: -115.5
In Glenfinnan, the Hogwarts Express crosses a viaduct, as it has in the past films. Aerial scenes were shot in Glen Coe, Clachaig Gully, and Glen Etive, which, at the time of filming, was one of the few places in Scotland without snow, making it ideal for a backdrop. Director David Yates stated in an interview that he had originally shot a three-hour cut of &quot;Order of the Phoenix&quot;.

Geographic entities mentioned:
surface_form: Glen Etive
instance_of: Valley
countries: United Kingdom
coordinates: lat: 56.601111111111
lon: -5.0058333333333
Black Creek is a tributary of the St. Johns River in Clay County, Florida. It is formed by the confluence of North Fork Black Creek and South Fork Black Creek. North Fork Black Creek originates as an outflow from Kingsley Lake and flows north and then southeast, meeting South Fork Black Creek on the east side of MIddleburg. North Fork Black Creek has Yellow Water Creek as its main tributary.

Geographic entities mentioned:
surface_form: Kingsley Lake
instance_of: Lake
countries: United States
coordinates: lat: 29.964722222222
lon: -81.998055555556
North Fork Black Creek. North Fork Black Creek arises as the outflow from Kingsley Lake. It runs northward and then turns to the southeast flowing through Jennings State Forest to its confluence with South Fork Black Creek near Middleburg. Its primary tributary is Yellow Water Creek, which arises in swamps in Duval County, flowing south to meet North Fork Black Creek in Jennings State Forest.

Geographic entities mentioned:
surface_form: Kingsley Lake
instance_of: Lake
countries: United States
coordinates: lat: 29.964722222222
lon: -81.998055555556
The desert rainbowfish (&quot;M. s. tatei&quot;) is endemic to the drainage basin of Lake Eyre. Habitat and biology. &quot;Melanotaenia splendida&quot; are normally found close to the surface of the deeper pools in small freshwater streams, they also occur in lakes and reservoirs.

Geographic entities mentioned:
surface_form: Lake Eyre
instance_of: Lake
countries: Australia
coordinates: lat: -28.406
lon: 137.2963
&quot;VC Unic Piatra Neamț&quot; is the local women's volleyball team. Piatra Neamț is the residence of &quot;Constantin &quot;Ticu&quot; Lăcătușu&quot;, the first Romanian alpinist who reached the top of Mount Everest. The Piatra Neamț Equestrian Stadium (&quot;Baza Hipică&quot;) is the host of several show jumping and dressage international competitions. Astronomical dedication.

Geographic entities mentioned:
surface_form: Mount Everest
instance_of: Mountain
countries: Nepal
People's Republic of China
coordinates: lat: 27.988055555555555
lon: 86.925
Occurrence. Shungite has mainly been found in Russia. The main deposit is in the Lake Onega area of Karelia, at Zazhoginskoye, near Shunga, with another occurrence at Vozhmozero. Two other much smaller occurrences have been reported in Russia, one in Kamchatka in volcanic rocks and the other formed by the burning of spoil from a coal mine at high temperature in Chelyabinsk.

Geographic entities mentioned:
surface_form: Lake Onega
instance_of: Lake
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 61.690555555556
lon: 35.655555555556
Scalation: 207–226 ventrals, 58–72 subcaudals, 23–29 scale rows around neck, 23–27 scale rows at midbody, 1–2 preoculars, 6–8 supralabials. Distribution. A scattered distribution in north-eastern Africa: Egypt (Nile Valley), Sudan (Nile Valley, Darfur), western Eritrea, Chad (Ennedi Plateau) and Niger (Aïr Mountains). Taxonomy.

Geographic entities mentioned:
surface_form: Ennedi Plateau
instance_of: Plateau
countries: Chad
coordinates: lat: 17
lon: 23
Hertha Nunatak. Hertha Nunatak () is a nunatak northwest of Castor Nunatak in the Seal Nunataks group, off the east coast of the Antarctic Peninsula.

Geographic entities mentioned:
surface_form: Castor Nunatak
instance_of: Mountain
coordinates: lat: -65.1667
lon: -59.9167
surface_form: Seal Nunataks
instance_of: Mountain
coordinates: lat: -65.03
lon: -60.05
surface_form: hertha nunatak
instance_of: Mountain
coordinates: lat: -65.15
lon: -59.9833
Hertha Nunatak. Hertha Nunatak () is a nunatak northwest of Castor Nunatak in the Seal Nunataks group, off the east coast of the Antarctic Peninsula.

Geographic entities mentioned:
surface_form: hertha nunatak
instance_of: Mountain
coordinates: lat: -65.15
lon: -59.9833
Planina, Ajdovščina. Planina () is a village in the hills south of the Vipava Valley on the border with the Karst Plateau in the Municipality of Ajdovščina in the traditional Inner Carniola region of Slovenia. It is now generally regarded as part of the Slovenian Littoral. It is made up of smaller clusters of the hamlets of Štrancarji, Marci, Dolenja Vas (), Brithi, Gorenja Vas (), and Koboli.

Geographic entities mentioned:
surface_form: Vipava Valley
instance_of: Valley
countries: Slovenia
coordinates: lat: 45.876147222222
lon: 13.907319444444
After the man died, Rae headed for Sault Ste. Marie in Ontario to find another instructor. The two-month, winter journey was by dog sled along the north shore of Lake Superior. From there, Sir George told him to go to Toronto to study under John Henry Lefroy at the Toronto Magnetic and Meteorological Observatory. Returning from Toronto, he received final instructions at Sault Ste. Marie.

Geographic entities mentioned:
surface_form: Lake Superior
instance_of: Lake
countries: Canada
United States
coordinates: lat: 47.52881611111111
lon: -87.76002194444445
Returning from Toronto, he received final instructions at Sault Ste. Marie. Rae finally departed on the voyage to Simpson's furthest-east on 5 August 1845, taking the usual voyageur route via Lake Winnipeg and reaching York Factory on 8 October, where he wintered. On 12 June 1846, he headed north in two boats and reached Repulse Bay at the south end of the Melville Peninsula in July.

Geographic entities mentioned:
surface_form: Lake Winnipeg
instance_of: Lake
countries: Canada
coordinates: lat: 52.116666666667
lon: -97.25
Rae's second journey began on 5 April 1847. He crossed to Committee Bay, travelled up its west coast for four days and then headed west across the base of the Simpson Peninsula to Pelly Bay. He went north and from a hill thought he could see Lord Mayor Bay, on the west side of the Gulf of Boothia, where John Ross had been trapped in ice from 1829 to 1833.

Geographic entities mentioned:
surface_form: Pelly Bay
instance_of: Body of water
countries: Canada
coordinates: lat: 68.8833
lon: -90.0833
Arctic coast. From 1848 to 1851, Rae made three journeys along the Arctic coast. The first took him from the Mackenzie River to the Coppermine River, which had been done before. On the second he tried to cross to Victoria Island but was blocked by ice. On the third he explored the whole south coast of Victoria Island.

Geographic entities mentioned:
surface_form: Coppermine River
instance_of: Watercourse
countries: Canada
coordinates: lat: 67.816666666667
lon: -115.06666666667
First journey. The Rae–Richardson Arctic Expedition left Liverpool in March 1848, reached New York, and took the usual voyageur routes west from Montreal. On 15 July 1848, the expedition reached Fort Resolution on Great Slave Lake. John Bell was sent downriver to establish winter quarters at Fort Confidence on the east arm of Great Bear Lake.

Geographic entities mentioned:
surface_form: Great Slave Lake
instance_of: Lake
countries: Canada
coordinates: lat: 61.666666666667
lon: -114
On 15 July 1848, the expedition reached Fort Resolution on Great Slave Lake. John Bell was sent downriver to establish winter quarters at Fort Confidence on the east arm of Great Bear Lake. Richardson and Rae traveled down the Mackenzie River and turned east along the coast.

Geographic entities mentioned:
surface_form: Great Bear Lake
instance_of: Lake
countries: Canada
coordinates: lat: 66
lon: -121
On 7 May, Richardson and Bell left with most of the men. Rae left on 9 June with seven men. Hauling a boat overland they reached the Kendall River on 21 June. The next day they reached the Coppermine River and waited a week for the ice to break up. They descended the Coppermine and waited again for the ice to clear on Coronation Gulf.

Geographic entities mentioned:
surface_form: Kendall River
instance_of: Watercourse
countries: Canada
coordinates: lat: 67.2
lon: -116.567
Rae left on 9 June with seven men. Hauling a boat overland they reached the Kendall River on 21 June. The next day they reached the Coppermine River and waited a week for the ice to break up. They descended the Coppermine and waited again for the ice to clear on Coronation Gulf. It was 30 July before they reached Cape Krusenstern on Coronation Gulf.

Geographic entities mentioned:
surface_form: Coppermine River
instance_of: Watercourse
countries: Canada
coordinates: lat: 67.816666666667
lon: -115.06666666667
He turned south, crossed Dolphin and Union Strait safely and on 5 June turned inland. The journey to camp on the Kendall River was the least pleasant part of the journey since he had to travel over melting snow and through meltwater. On 15 June 1851, two days after the boat arrived, he set off down the Kendall River and Coppermine River with 10 men.

Geographic entities mentioned:
surface_form: Kendall River
instance_of: Watercourse
countries: Canada
coordinates: lat: 67.2
lon: -116.567
Judging that it was too late to drag the boat north to the Back River, he turned back and wintered at his old camp on Repulse Bay. He left Repulse Bay on 31 March 1854. Near Pelly Bay he met some Inuit, one of whom had a gold cap-band. Asked where he got it, he replied that it came from a place 10 to 12 days away where 35 or so &quot;kabloonat&quot; had starved to death.

Geographic entities mentioned:
surface_form: Pelly Bay
instance_of: Body of water
countries: Canada
coordinates: lat: 68.8833
lon: -90.0833
The ship was built at Kingston, Canada West. Rae moved to Hamilton, Canada West, also on Lake Ontario, in 1857, where his two brothers lived and operated a shipping firm on the Great Lakes. The &quot;Iceberg&quot; was launched in 1857. Rae intended to sail her to England the following year to be outfitted for polar voyages. In the meantime, she was put to use as a cargo ship.

Geographic entities mentioned:
surface_form: Lake Ontario
instance_of: Lake
countries: Canada
United States
coordinates: lat: 43.72888888888889
lon: -78.10638888888889