Sarmila/GeoWiki-Features huggingface dataset:
The main rivers are the Amur, Amgun, Uda, and Tugur, among others. There are also lakes such as Bokon, Bolon, Chukchagir, Evoron, Kizi, Khummi, Orel, and Udyl, among others. Khabarovsk Krai has a severely continental climate with its northern areas being subarctic with stronger maritime summer moderation in the north.

Geographic entities mentioned:
surface_form: Bokon
instance_of: Lake
countries: Russia
Soviet Union
Russian Empire
coordinates: lat: 54.328888888889
lon: 134.17
surface_form: Bolon
instance_of: Lake
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 49.861447222222
lon: 136.46530277778
surface_form: Evoron
instance_of: Lake
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 51.44
lon: 136.52638888889
surface_form: Kizi
instance_of: Lake
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 51.616666666667
lon: 140.48333333333
surface_form: Khummi
instance_of: Lake
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 50.328888888889
lon: 137.295
surface_form: Orel
instance_of: Lake
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 53.465555555556
lon: 139.72638888889
surface_form: Udyl
instance_of: Lake
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 52.144722222222
lon: 139.88944444444
The main mountain ranges in the region are the Bureya Range, the Badzhal Range (highest point high, the Gora Ulun), the Yam-Alin, the Dusse-Alin, the Sikhote-Alin, the Dzhugdzhur Mountains, the Kondyor Massif, as well as a small section of the Suntar-Khayata Range, the Yudoma-Maya Highlands, and the Sette-Daban in the western border regions. The highest point is high, Berill Mountain.

Geographic entities mentioned:
surface_form: Gora Ulun
instance_of: Mountain
countries: Russia
Soviet Union
Russian Empire
coordinates: lat: 50.508888888889
lon: 134.32638888889
The main mountain ranges in the region are the Bureya Range, the Badzhal Range (highest point high, the Gora Ulun), the Yam-Alin, the Dusse-Alin, the Sikhote-Alin, the Dzhugdzhur Mountains, the Kondyor Massif, as well as a small section of the Suntar-Khayata Range, the Yudoma-Maya Highlands, and the Sette-Daban in the western border regions. The highest point is high, Berill Mountain.

Geographic entities mentioned:
surface_form: Berill Mountain
instance_of: Mountain
countries: Russia
Soviet Union
Russian Empire
coordinates: lat: 62.395833333333
lon: 141.32666666667
The company's first beer was brewed on 15 December 1922. The first batch was delivered to the Stanley Hotel, where it received mixed reactions. Originally brewed in Kenya, the beer expaded to Tanzania and other countries in the African Great Lakes region, and was eventually exported. The company's first annual general meeting was held in 1923.

Geographic entities mentioned:
surface_form: African Great Lakes
instance_of: Group of lakes
countries: Burundi
Zambia
Kenya
Democratic Republic of the Congo
Malawi
Mozambique
Rwanda
Tanzania
Uganda
Ethiopia
coordinates: lat: -8
lon: 35
Lake Bolluk. Lake Bolluk is a lake in Turkey. The lake is in Cihanbeyli ilçe (district) of Konya Province. It is situated to the east of the highway D.715, which connects Ankara to Silifke and to the west of Lake Tuz. The area of the lake is. Its elevation with respect to sea level is. The hard water of the lake contains sodium.

Geographic entities mentioned:
surface_form: lake bolluk
instance_of: Lake
countries: Turkey
coordinates: lat: 38.5217
lon: 32.9269
In 1963, Caldwell Township changed its name to Fairfield in order to avoid being confused with Caldwell Borough. Immediately following the separation of the original Caldwell, the western part of Caldwell Borough generally remained less developed than downtown Caldwell Borough and contained several farms and a large area of undeveloped swampland known as Hatfield Swamp.

Geographic entities mentioned:
surface_form: Hatfield Swamp
instance_of: Landform
countries: United States
coordinates: lat: 40.8408
lon: -74.3283
Caribou Island (near Michipicoten Island). Caribou Island is an uninhabited island in the eastern end of Lake Superior, south of Michipicoten Island. It lies entirely within the territorial waters of Canada although only about five kilometres from the international border between Canada and the United States. It is approximately long and wide, and in area.

Geographic entities mentioned:
surface_form: Lake Superior
instance_of: Lake
countries: Canada
United States
coordinates: lat: 47.52881611111111
lon: -87.76002194444445
It is approximately long and wide, and in area. The interior is low scrub and bog with small lakes, Little Italy, Hambone, and Deer Lake among many unnamed ones. Several of the lakes are maintained by beavers and all are several feet above Lake Superior. History.

Geographic entities mentioned:
surface_form: Lake Superior
instance_of: Lake
countries: Canada
United States
coordinates: lat: 47.52881611111111
lon: -87.76002194444445
Marie, Ontario, only about 80–90 miles SE. However an interior lake, Deer Lake on the center East side of the island, was used as an Amphibian base with a dock and ramp built by the last private owners of the island because of the unpredictable water/wave condition of Lake Superior. A small three room cabin was built on the east shore of Lake Superior adjacent to Deer Lake and the Amphibian base.

Geographic entities mentioned:
surface_form: Lake Superior
instance_of: Lake
countries: Canada
United States
coordinates: lat: 47.52881611111111
lon: -87.76002194444445
Purvanchal Range. The Purvanchal Range, or the Eastern Highlands, refers to the northern portion of the Indo-Burman Ranges. It extends through the northeast Indian states of Arunachal Pradesh, Nagaland, Manipur, Tripura and Mizoram. Geography.

Geographic entities mentioned:
surface_form: Indo-Burman Ranges
instance_of: Mountain
coordinates: lat: 23.666666666666668
lon: 94.16666666666667
The range is the northern portion of the Indo-Burman Range, in north eastern India. It bends sharply to the south beyond the Dihang River gorge, and spreads along the eastern boundary of India with Myanmar. The Purvanchal includes the hill of the Patkai hills, Naga Hills, Mizo Hills and Manipur hills. Geology. The Purvanchal Mountains are composed largely of strong sandstone geological formations

Geographic entities mentioned:
surface_form: Naga Hills
instance_of: Mountain
countries: Myanmar
India
coordinates: lat: 26
lon: 95
It also includes The Musical Stones of Skiddaw, a number of lithophones built across two centuries around the town of Keswick using hornfels, a stone from the nearby Skiddaw mountain, which is said to have a superior tone and longer ring than the more commonly used slate.

Geographic entities mentioned:
surface_form: Skiddaw
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.651388888889
lon: -3.1477777777778
The salt water inlet changed into a fresh water lake now called the IJsselmeer (IJssel Lake) after the river that drains into it, and by means of drainage and polders, an area of some was reclaimed as land. This land eventually became the province of Flevoland. Part of the IJsselmeer was also divided into the Markermeer. Lake Flevo.

Geographic entities mentioned:
surface_form: Markermeer
instance_of: Lake
countries: Netherlands
coordinates: lat: 52.566666666667
lon: 5.2166666666667
Resurrection Peaks. Resurrection Peaks is a mountain ridge located in the Kenai Mountains, on the Kenai Peninsula, in the U.S. state of Alaska. The peaks are situated in Chugach National Forest, north of Mount Benson, south of Mount Ascension, and north of Seward, Alaska. These peaks, marked 4712' and 4665' on the USGS map, together with their ridges and glacier form a distinct group.

Geographic entities mentioned:
surface_form: Mount Ascension
instance_of: Mountain
countries: United States
coordinates: lat: 60.259166666666665
lon: -149.4958333333333
Sentob. Sentob, also Sentyab or Sintab (;), is an Uzbek village in Nurota District, Navoiy Region of Uzbekistan. The settlement is nestled 30 km south of the Aydar Lake 6 km into a fertile green river valley of the Nuratau Mountains. It is situated at an elevation of 600 m and the town population is about 1,000 people. Description of the village.

Geographic entities mentioned:
surface_form: Aydar Lake
instance_of: Lake
countries: Uzbekistan
Russian Empire
Soviet Union
coordinates: lat: 40.89
lon: 66.92
Awach Tende. Awach Tende is a settlement in Kenya's Homa Bay County. Awach Tende is also the name of a river in the Lake Victoria catchment area. Along with Awach Kibuon, it is known as South Awach. History. Before the Kenyan general election in 2013, Awach voted as part of the Nyanza Province.

Geographic entities mentioned:
surface_form: Lake Victoria
instance_of: Lake
countries: Tanzania
Uganda
Kenya
coordinates: lat: -1
lon: 33
Canopus Rocks. The Canopus Rocks are two small, low rocks lying northwest of Canopus Island, east of Nella Rock and the Sawert Rocks, and southeast of Hansen Rocks in the eastern part of Holme Bay, Mac. Robertson Land.

Geographic entities mentioned:
surface_form: Nella Rock
instance_of: Landform
coordinates: lat: -67.5167
lon: 62.85
It is southwest of the town of Telluride and is named for a prominent rock formation that is said to look like a lizard's head. Lizard Head itself is and is a volcanic spire of crumbling rock. Due to the steepness of the cliffs and the poor quality of the rock for fixing ropes, only experienced mountaineers should attempt to summit the spire.

Geographic entities mentioned:
surface_form: Lizard Head
instance_of: Mountain
countries: United States
coordinates: lat: 37.835827777778
lon: -107.95062222222
Another of trails in this infrequently visited wilderness, are also strenuous and should be attempted by more advanced backpackers. The area includes three prominent fourteeners: El Diente Peak (), Wilson Peak (), and Mount Wilson (). The area includes the headwaters of the west fork of the Dolores River.

Geographic entities mentioned:
surface_form: El Diente Peak
instance_of: Mountain
countries: United States
coordinates: lat: 37.839444444444
lon: -108.00527777778
surface_form: Wilson Peak
instance_of: Mountain
countries: United States
coordinates: lat: 37.8603
lon: -107.985
Guayuriba River. Guayuriba River is a river of Colombia. It is part of the Orinoco River basin.

Geographic entities mentioned:
surface_form: guayuriba river
instance_of: Watercourse
countries: Colombia
coordinates: lat: 3.9080555555555554
lon: -73.09472222222222
The district also contains the Dells of the Wisconsin River State Natural Area, Mirror Lake State Park, Dell Creek State Wildlife Area, the Mt. Olympus Water & Theme Park, and the Noah's Ark Water Park. The seat is represented by Republican Tony Kurtz since January 2025; Kurtz previously represented the 50th district from 2019 to 2025.

Geographic entities mentioned:
surface_form: Mirror Lake State Park
instance_of: Lake
countries: United States
coordinates: lat: 43.565
lon: -89.82
Rowing at the 1936 Summer Olympics – Men's coxed pair. The men's coxed pair competition at the 1936 Summer Olympics in Berlin took place at Grünau on the Langer See. It was held from 12 to 14 August. There were 12 boats (36 competitors) from 12 nations, with each nation limited to a single boat in the event.

Geographic entities mentioned:
surface_form: Langer See
instance_of: Lake
countries: Germany
coordinates: lat: 52.4052
lon: 13.6271
Mount Edziza. Mount Edziza (;) is a volcanic mountain in Cassiar Land District of northwestern British Columbia, Canada. It is located on the Big Raven Plateau of the Tahltan Highland which extends along the western side of the Stikine Plateau. Mount Edziza has an elevation of, making it the highest point of the Mount Edziza volcanic complex and one of the highest volcanoes in Canada.

Geographic entities mentioned:
surface_form: Big Raven Plateau
instance_of: Plateau
countries: Canada
coordinates: lat: 57.7167
lon: -130.75
surface_form: Stikine Plateau
instance_of: Plateau
countries: Canada
coordinates: lat: 58.38305555555556
lon: -129.885
Mount Edziza. Mount Edziza (;) is a volcanic mountain in Cassiar Land District of northwestern British Columbia, Canada. It is located on the Big Raven Plateau of the Tahltan Highland which extends along the western side of the Stikine Plateau. Mount Edziza has an elevation of, making it the highest point of the Mount Edziza volcanic complex and one of the highest volcanoes in Canada.

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: 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
The mountain contains several lava domes, cinder cones and lava fields on its flanks, as well as an ice cap containing several outlet glaciers which extend to lower elevations. All sides of Mount Edziza are drained by tributaries of Mess Creek and Kakiddi Creek which are situated within the Stikine River watershed.

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: 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
The first stage 1.1 million years ago produced basalt flows and a series of rhyolite and trachyte domes. Basalt flows and smaller amounts of trachyte, tristanite, trachybasalt, benmoreite and mugearite produced during the second stage about 1 million years ago comprise Ice Peak, a glacially eroded stratovolcano forming the south peak of Mount Edziza.

Geographic entities mentioned:
surface_form: Ice Peak
instance_of: Mountain
countries: Canada
coordinates: lat: 57.6906
lon: -130.635
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
A 1927 report by J. Davidson of the British Columbia Land Surveyors claims that &quot;Edziza&quot; means 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. According to David Stevenson of University of Victoria's Anthropology Department, or is instead translated as in Tahltan.

Geographic entities mentioned:
surface_form: Big Raven Plateau
instance_of: Plateau
countries: Canada
coordinates: lat: 57.7167
lon: -130.75
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: big raven plateau
instance_of: Plateau
countries: Canada
coordinates: lat: 57.7167
lon: -130.75
Location and climate. Mount Edziza rises from within the middle of the Big Raven Plateau, a barren plateau in Cassiar Land District bounded on the west by Mess Valley, on the north by Klastline Valley, on the east by Kakiddi Valley and on the south by Chakima and Walkout valleys.

Geographic entities mentioned:
surface_form: Chakima
instance_of: Watercourse
countries: Canada
coordinates: lat: 57.59966
lon: -130.42066
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
Mount Edziza rises from within the middle of the Big Raven Plateau, a barren plateau in Cassiar Land District bounded on the west by Mess Valley, on the north by Klastline Valley, on the east by Kakiddi Valley and on the south by Chakima and Walkout valleys. It lies at the northern end of the Mount Edziza volcanic complex which also includes the smaller Arctic Lake and Kitsu plateaus to the south.

Geographic entities mentioned:
surface_form: Mount Edziza volcanic complex
instance_of: Mountain
countries: Canada
coordinates: lat: 57.5
lon: -130.6
surface_form: Arctic Lake
instance_of: Plateau
countries: Canada
coordinates: lat: 57.3
lon: -130.767
surface_form: Kitsu
instance_of: Plateau
countries: Canada
coordinates: lat: 57.4667
lon: -130.75
This complex of shield volcanoes, stratovolcanoes, lava domes, calderas and cinder cones forms a broad, intermontane plateau at the eastern edge of the Tahltan Highland, a southeast-trending upland area extending along the western side of the Stikine Plateau.

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
The Mount Edziza glacier complex is the only one worthy of note on the Stikine Plateau. Four outlet glaciers of the ice cap are named, and all have names of Tahltan origin. Idiji Glacier descends from the eastern side of the ice cap near the head of Tennaya Creek. At the head of Tenchen Creek is Tenchen Glacier, a debris-covered glacier on the eastern side of the ice cap.

Geographic entities mentioned:
surface_form: Tennaya Creek
instance_of: Watercourse
countries: Canada
coordinates: lat: 57.69966
lon: -130.42065
Four outlet glaciers of the ice cap are named, and all have names of Tahltan origin. Idiji Glacier descends from the eastern side of the ice cap near the head of Tennaya Creek. At the head of Tenchen Creek is Tenchen Glacier, a debris-covered glacier on the eastern side of the ice cap. Tencho Glacier at the southern end of the ice cap is the largest outlet glacier.

Geographic entities mentioned:
surface_form: Tenchen Creek
instance_of: Watercourse
countries: Canada
coordinates: lat: 57.76636
lon: -130.43724
Structure. Mount Edziza has an elevation of, making it the highest point of the Mount Edziza volcanic complex. It has been considered by some to be the highest or tallest volcano in Canada, but others have given higher elevations of for the Silverthrone volcanic complex in southwestern British Columbia.

Geographic entities mentioned:
surface_form: Silverthrone
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4333
lon: -126.3
surface_form: columbia
instance_of: Mountain
countries: Canada
coordinates: lat: 52.1475
lon: -117.44055555555556
Although Mount Edziza is surrounded by relatively flat terrain of the Big Raven Plateau to the north, west and south, the terrain east of the mountain is characterized by a series of ridges with intervening valleys. Among these ridges are Idiji Ridge and Sorcery Ridge which are the namesakes of Idiji Glacier and Sorcery Creek. About south of the summit is Ice Peak, the south peak of Mount Edziza.

Geographic entities mentioned:
surface_form: Idiji Ridge
instance_of: Mountain
coordinates: lat: 57.67653055555555
lon: -130.6231527777778
surface_form: Sorcery Ridge
instance_of: Mountain
coordinates: lat: 57.65606944444444
lon: -130.61504166666666
Among these ridges are Idiji Ridge and Sorcery Ridge which are the namesakes of Idiji Glacier and Sorcery Creek. About south of the summit is Ice Peak, the south peak of Mount Edziza. This prominent pyramid-shaped horn has an elevation of and is the glacially eroded remains of an older stratovolcano whose northern flank is buried under the younger edifice of Mount Edziza.

Geographic entities mentioned:
surface_form: Ice Peak
instance_of: Mountain
countries: Canada
coordinates: lat: 57.6906
lon: -130.635
Subfeatures. High on the eastern rim of Ice Peak are two glaciated volcanic cones called Icefall Cone and Ridge Cone, both with elevations of about. Punch Cone on the western flank of Ice Peak protrudes through Mount Edziza's ice cap whereas Koosick Bluff and Ornostay Bluff, also on the western flank of Ice Peak, extend westward onto the surrounding Big Raven Plateau.

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: 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
surface_form: big raven plateau
instance_of: Plateau
countries: Canada
coordinates: lat: 57.7167
lon: -130.75
The northeastern side of Mount Edziza contains The Pyramid, a pyramid-shaped lava dome in elevation. Pillow Ridge on the northern side of Mount Edziza has an elevation of whereas Tsekone Ridge northwest of Mount Edziza has an elevation of. High on the western side of Mount Edziza is Triangle Dome, an elliptical lava dome in elevation.

Geographic entities mentioned:
surface_form: Pillow Ridge
instance_of: Mountain
countries: Canada
coordinates: lat: 57.7594
lon: -130.652
surface_form: Tsekone Ridge
instance_of: Mountain
countries: Canada
coordinates: lat: 57.77
lon: -130.69
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
High on the western side of Mount Edziza is Triangle Dome, an elliptical lava dome in elevation. Glacier Dome reaches an elevation of on Mount Edziza's lower northeastern flank. A circular lava dome on the southeastern crater rim of Mount Edziza called Nanook Dome has an elevation of. Sphinx Dome, in elevation, is a partially buried lava dome on the northeastern flank of Mount Edziza.

Geographic entities mentioned:
surface_form: Glacier Dome
instance_of: Mountain
countries: Canada
coordinates: lat: 56.4029
lon: -130.9166
The Neck, in elevation, is a circular volcanic plug on the southeastern flank of Ice Peak. The Snowshoe Lava Field on the west flank of lce Peak contains at least 12 volcanic cones, a handful of which are named. Tennena Cone is a symmetrical volcanic cone high on the west side of Ice Peak. It has an elevation of and is almost completely surrounded by ice.

Geographic entities mentioned:
surface_form: Tennena Cone
instance_of: Mountain
countries: Canada
coordinates: lat: 57.68416666666667
lon: -130.66222222222223
Tennena Cone is a symmetrical volcanic cone high on the west side of Ice Peak. It has an elevation of and is almost completely surrounded by ice. Cocoa Crater is the largest cone in the Snowshoe Lava Field and is in elevation. To the southeast is Coffee Crater which has an elevation of. Keda Cone, in elevation, lies just south of Coffee Crater on the south side of upper Taweh Creek.

Geographic entities mentioned:
surface_form: Cocoa Crater
instance_of: Mountain
countries: Canada
coordinates: lat: 57.65
lon: -130.7
It has an elevation of and is almost completely surrounded by ice. Cocoa Crater is the largest cone in the Snowshoe Lava Field and is in elevation. To the southeast is Coffee Crater which has an elevation of. Keda Cone, in elevation, lies just south of Coffee Crater on the south side of upper Taweh Creek. A saucer-shaped mound of lava called The Saucer is in elevation and has a diameter of about.

Geographic entities mentioned:
surface_form: Coffee Crater
instance_of: Mountain
countries: Canada
coordinates: lat: 57.63
lon: -130.67
It has an elevation of and is almost completely surrounded by ice. Cocoa Crater is the largest cone in the Snowshoe Lava Field and is in elevation. To the southeast is Coffee Crater which has an elevation of. Keda Cone, in elevation, lies just south of Coffee Crater on the south side of upper Taweh Creek. A saucer-shaped mound of lava called The Saucer is in elevation and has a diameter of about.

Geographic entities mentioned:
surface_form: Taweh Creek
instance_of: Watercourse
countries: Canada
coordinates: lat: 57.71638
lon: -130.97063
Twin Cone, in elevation, is a pyroclastic cone whose southeastern side has been breached. Moraine Cone has an elevation of nearly and has been nearly destroyed by alpine glaciation. The northeastern side of Mount Edziza contains Williams Cone, a prominent cinder cone in elevation. Eve Cone, in elevation, is a symmetrical cone between Buckley Lake and Mount Edziza.

Geographic entities mentioned:
surface_form: Williams Cone
instance_of: Mountain
countries: Canada
coordinates: lat: 57.78
lon: -130.599
surface_form: cinder cone
instance_of: Mountain
countries: Canada
coordinates: lat: 49.9717
lon: -123.007
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
The northeastern side of Mount Edziza contains Williams Cone, a prominent cinder cone in elevation. Eve Cone, in elevation, is a symmetrical cone between Buckley Lake and Mount Edziza. The northernmost cinder cone in the Desolation Lava Field is Sidas Cone which consists of two symmetrical halves and reaches an elevation of. Drainage.

Geographic entities mentioned:
surface_form: Eve Cone
instance_of: Mountain
countries: Canada
coordinates: lat: 57.81305555555556
lon: -130.67555555555555
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
The northeastern side of Mount Edziza contains Williams Cone, a prominent cinder cone in elevation. Eve Cone, in elevation, is a symmetrical cone between Buckley Lake and Mount Edziza. The northernmost cinder cone in the Desolation Lava Field is Sidas Cone which consists of two symmetrical halves and reaches an elevation of. Drainage.

Geographic entities mentioned:
surface_form: Sidas Cone
instance_of: Mountain
countries: Canada
coordinates: lat: 57.8589
lon: -130.628
Drainage. Mount Edziza is drained on all sides by streams within the Stikine River watershed. Elwyn Creek is a westward-flowing stream originating from the northwestern flank of Mount Edziza. It contains one named tributary, Kadeya Creek, which flows northwest from Mount Edziza. Sezill Creek is a westward-flowing stream originating from the western flank of Mount Edziza.

Geographic entities mentioned:
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instance_of: Watercourse
countries: Canada
coordinates: lat: 57.78298
lon: -130.98722
surface_form: edziza
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countries: Canada
coordinates: lat: 57.715555555555554
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instance_of: Mountain
countries: Canada
coordinates: lat: 57.715555555555554
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Drainage. Mount Edziza is drained on all sides by streams within the Stikine River watershed. Elwyn Creek is a westward-flowing stream originating from the northwestern flank of Mount Edziza. It contains one named tributary, Kadeya Creek, which flows northwest from Mount Edziza. Sezill Creek is a westward-flowing stream originating from the western flank of Mount Edziza.

Geographic entities mentioned:
surface_form: Kadeya Creek
instance_of: Watercourse
countries: Canada
coordinates: lat: 57.79967
lon: -130.87063
surface_form: edziza
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countries: Canada
coordinates: lat: 57.715555555555554
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countries: Canada
coordinates: lat: 57.715555555555554
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Elwyn Creek is a westward-flowing stream originating from the northwestern flank of Mount Edziza. It contains one named tributary, Kadeya Creek, which flows northwest from Mount Edziza. Sezill Creek is a westward-flowing stream originating from the western flank of Mount Edziza. It is a tributary of Taweh Creek which flows northwest from just south of Mount Edziza.

Geographic entities mentioned:
surface_form: Sezill Creek
instance_of: Watercourse
countries: Canada
coordinates: lat: 57.69967
lon: -130.88724
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countries: Canada
coordinates: lat: 57.715555555555554
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surface_form: mount edziza
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countries: Canada
coordinates: lat: 57.715555555555554
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Sezill Creek is a westward-flowing stream originating from the western flank of Mount Edziza. It is a tributary of Taweh Creek which flows northwest from just south of Mount Edziza. Elwyn Creek and Taweh Creek are tributaries of Mess Creek which flows northwestward into the Stikine River. Tsecha Creek is a northeast-flowing stream originating from the northern flank of Mount Edziza.

Geographic entities mentioned:
surface_form: Mess Creek
instance_of: Watercourse
countries: Canada
coordinates: lat: 57.88296
lon: -131.2206
It is a tributary of Taweh Creek which flows northwest from just south of Mount Edziza. Elwyn Creek and Taweh Creek are tributaries of Mess Creek which flows northwestward into the Stikine River. Tsecha Creek is a northeast-flowing stream originating from the northern flank of Mount Edziza. Nido Creek flows northeastward from the eastern side of Mount Edziza into Nuttlude Lake.

Geographic entities mentioned:
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instance_of: Watercourse
countries: Canada
coordinates: lat: 57.83296
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countries: Canada
coordinates: lat: 57.715555555555554
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countries: Canada
coordinates: lat: 57.715555555555554
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Elwyn Creek and Taweh Creek are tributaries of Mess Creek which flows northwestward into the Stikine River. Tsecha Creek is a northeast-flowing stream originating from the northern flank of Mount Edziza. Nido Creek flows northeastward from the eastern side of Mount Edziza into Nuttlude Lake. Flowing from the eastern flank of Mount Edziza just southeast of The Pyramid is Tenchen Creek.

Geographic entities mentioned:
surface_form: Nido Creek
instance_of: Watercourse
countries: Canada
coordinates: lat: 57.71636
lon: -130.47065
Nido Creek flows northeastward from the eastern side of Mount Edziza into Nuttlude Lake. Flowing from the eastern flank of Mount Edziza just southeast of The Pyramid is Tenchen Creek. Shaman Creek flows east and north into Kakiddi Lake from the southern flank of Mount Edziza. Tennaya Creek flows northeastward from the eastern side of Mount Edziza into Nuttlude Lake.

Geographic entities mentioned:
surface_form: Shaman Creek
instance_of: Watercourse
countries: Canada
coordinates: lat: 57.61636
lon: -130.40395
Shaman Creek flows east and north into Kakiddi Lake from the southern flank of Mount Edziza. Tennaya Creek flows northeastward from the eastern side of Mount Edziza into Nuttlude Lake. All five streams are tributaries of Kakiddi Creek, a north-flowing tributary of the Klastline River which flows north into the Stikine River. Background.

Geographic entities mentioned:
surface_form: Kakiddi Creek
instance_of: Watercourse
countries: Canada
coordinates: lat: 57.872778
lon: -130.425556
All five streams are tributaries of Kakiddi Creek, a north-flowing tributary of the Klastline River which flows north into the Stikine River. Background. Mount Edziza is part of the Northern Cordilleran Volcanic Province, 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
Hazards and monitoring. A Natural Resources Canada report published in 2021 considers Mount Edziza a high threat volcano because it has had the highest eruption rate in Canada throughout the Holocene. However, its extremely remote location makes it less hazardous than Mount Garibaldi, Mount Price, Mount Cayley and Mount Meager in southwestern British Columbia.

Geographic entities mentioned:
surface_form: Mount Garibaldi
instance_of: Mountain
countries: Canada
coordinates: lat: 49.850555555556
lon: -123.00472222222
However, its extremely remote location makes it less hazardous than Mount Garibaldi, Mount Price, Mount Cayley and Mount Meager in southwestern British Columbia. The hazard rating of Mount Edziza is similar to that of Mount Churchill in the U.S. state of Alaska which deposited the White River Ash across northwestern Canada in the last 2,000 years.

Geographic entities mentioned:
surface_form: Mount Churchill
instance_of: Mountain
countries: United States
coordinates: lat: 61.41916666666667
lon: -141.71527777777777
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
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Sorcery Ridge obsidian occurs in at least two archaeological sites outside of Tahltan territory. In or before 1974, two Tahltan men named Johnny Edzerza and Hank Williams were killed in an avalanche while they were crossing the mountain. Edzerza was buried on Mount Edziza, but his surname was erroneously spelled &quot;Edzertza&quot; on his grave marker.

Geographic entities mentioned:
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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
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 Mount Edziza. 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 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
surface_form: buckley lake
instance_of: Lake
countries: Canada
coordinates: lat: 44.41806
lon: -78.2298
surface_form: buckley lake
instance_of: Lake
countries: Canada
coordinates: lat: 44.41806
lon: -78.2298
Stratigraphy. Mount Edziza is subdivided into at least six geological formations, each the product of a distinct stage of volcanic activity. These periods of volcanic activity occurred during four magmatic cycles of the Mount Edziza volcanic complex; each cycle began with the effusion of alkali basalt and culminated with the eruption of lesser volumes of felsic magma.

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
The oldest geological formation comprising Mount Edziza is the Pyramid Formation, which formed during a period of volcanic activity 1.1 million years ago at the end of the second magmatic cycle. Another period of volcanic activity about 1 million years ago during the start of the third magmatic cycle deposited the Ice Peak Formation on the southern part of the Pyramid Formation.

Geographic entities mentioned:
surface_form: the pyramid
instance_of: Mountain
countries: Canada
coordinates: lat: 57.7628
lon: -130.564
The youngest geological formation is the Big Raven Formation, which was formed by a period of volcanic activity during the fifth magmatic cycle in the last 20,000 years. Pyramid Formation. The Pyramid Formation is exposed along the deeply eroded eastern flank of Mount Edziza where rhyolite and trachyte flows, domes and pyroclastic rocks of this formation comprise ridges and prominent cliffs.

Geographic entities mentioned:
surface_form: the pyramid
instance_of: Mountain
countries: Canada
coordinates: lat: 57.7628
lon: -130.564
A basaltic lava flow sequence up to thick overlies the basal trachytic surge deposit of the Pyramid Formation; it is included as a part of this formation due to it being coeval with the early stages of Pyramid felsic volcanism.

Geographic entities mentioned:
surface_form: the pyramid
instance_of: Mountain
countries: Canada
coordinates: lat: 57.7628
lon: -130.564
Potassium–argon dating of the Pyramid Formation has yielded ages of 1.2 ± 0.4 million years and 1.2 ± 0.03 million years from comenditic glass, as well as 0.94 ± 0.12 million years and 0.94 ± 0.05 million years from trachyte. The Pyramid Formation includes Sphinx Dome, Pharaoh Dome and The Pyramid which were the main sources of the rhyolites and trachytes of this geological formation.

Geographic entities mentioned:
surface_form: the pyramid
instance_of: Mountain
countries: Canada
coordinates: lat: 57.7628
lon: -130.564
surface_form: the pyramid
instance_of: Mountain
countries: Canada
coordinates: lat: 57.7628
lon: -130.564
Potassium–argon dating of the Pyramid Formation has yielded ages of 1.2 ± 0.4 million years and 1.2 ± 0.03 million years from comenditic glass, as well as 0.94 ± 0.12 million years and 0.94 ± 0.05 million years from trachyte. The Pyramid Formation includes Sphinx Dome, Pharaoh Dome and The Pyramid which were the main sources of the rhyolites and trachytes of this geological formation.

Geographic entities mentioned:
surface_form: the pyramid
instance_of: Mountain
countries: Canada
coordinates: lat: 57.7628
lon: -130.564
Both bluffs are similar in geomorphology and composition, consisting of several lava flows up to thick. The Neck, which forms a prominent high buttress on Sorcery Ridge, is also part of the Ice Peak Formation. Potassium–argon dating of pantelleritic trachyte from the Ice Peak Formation has yielded ages of 1.6 ± 0.2 million years, 1.5 ± 0.4 million years and 1.5 ± 0.1 million years.

Geographic entities mentioned:
surface_form: ice peak
instance_of: Mountain
countries: Canada
coordinates: lat: 57.6906
lon: -130.635
surface_form: ice peak
instance_of: Mountain
countries: Canada
coordinates: lat: 57.6906
lon: -130.635
Glacier Dome reaches an elevation of on Mount Edziza's lower northeastern flank. A circular lava dome on the southeastern crater rim of Mount Edziza called Nanook Dome has an elevation of. Sphinx Dome, in elevation, is a partially buried lava dome on the northeastern flank of Mount Edziza. Remnants of a volcanic pile called Pharaoh Dome occur along the eastern flank of Mount Edziza.

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
Tsecha Creek is a northeast-flowing stream originating from the northern flank of Mount Edziza. Nido Creek flows northeastward from the eastern side of Mount Edziza into Nuttlude Lake. Flowing from the eastern flank of Mount Edziza just southeast of The Pyramid is Tenchen Creek. Shaman Creek flows east and north into Kakiddi Lake from the southern flank of Mount Edziza.

Geographic entities mentioned:
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
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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
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The Pyramid is a prominent trachyte dome whose structure has not been greatly modified by erosion, nor has it been buried under younger lavas. In contrast, much of the southern edge of Sphinx Dome has been destroyed by headward erosion of Cook Creek; the western half of this rhyolite dome is also buried under trachyte of the Edziza Formation.

Geographic entities mentioned:
surface_form: edziza
instance_of: Mountain
countries: Canada
coordinates: lat: 57.715555555555554
lon: -130.63472222222222
Accessibility. Mount Edziza lies in a remote location that is accessible only during summer and early autumn. There is no established road access to the mountain, although the Stewart–Cassiar Highway to the east and the Telegraph Creek Road to the northwest both come within of Mount Edziza. Extending from these roads are horse trails that provide access to the mountain.

Geographic entities mentioned:
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
Extending from these roads are horse trails that provide access to the mountain. 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
surface_form: buckley lake
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countries: Canada
coordinates: lat: 44.41806
lon: -78.2298
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instance_of: Lake
countries: Canada
coordinates: lat: 44.41806
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The Buckley Lake to Mowdade Lake Route traverses south from Buckley Lake along Buckley Creek and gradually climbs onto the northern end of the Big Raven 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
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countries: Canada
coordinates: lat: 57.905833
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surface_form: buckley lake
instance_of: Lake
countries: Canada
coordinates: lat: 44.41806
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countries: Canada
coordinates: lat: 44.41806
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surface_form: tsekone ridge
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countries: Canada
coordinates: lat: 57.77
lon: -130.69
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instance_of: Mountain
countries: Canada
coordinates: lat: 57.77
lon: -130.69
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
surface_form: buckley lake
instance_of: Lake
countries: Canada
coordinates: lat: 44.41806
lon: -78.2298
Mount Edziza. Mount Edziza (;) is a volcanic mountain in Cassiar Land District of northwestern British Columbia, Canada. It is located on the Big Raven Plateau of the Tahltan Highland which extends along the western side of the Stikine Plateau. Mount Edziza has an elevation of, making it the highest point of the Mount Edziza volcanic complex and one of the highest volcanoes in Canada.

Geographic entities mentioned:
surface_form: columbia
instance_of: Mountain
countries: Canada
coordinates: lat: 52.1475
lon: -117.44055555555556
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: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
On December 3, 1974, the form of name was changed from &quot;Edziza Peak&quot; to &quot;Mount Edziza&quot; in accordance with a 1927 British Columbia Land Surveyors report, two world aeronautical charts published in 1950, and three British Columbia maps published in 1931, 1933 and 1943.

Geographic entities mentioned:
surface_form: columbia
instance_of: Mountain
countries: Canada
coordinates: lat: 52.1475
lon: -117.44055555555556
surface_form: columbia
instance_of: Mountain
countries: Canada
coordinates: lat: 52.1475
lon: -117.44055555555556
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
The form of the name was also changed to reflect entrenched local usage and in conformation with Mount Edziza Provincial Park, which was established in 1972. To the local Tahltan people, Mount Edziza is called, which translates to. A number of explanations have been made regarding the origin of the name &quot;Edziza&quot;. A 1927 report by J.

Geographic entities mentioned:
surface_form: edziza
instance_of: Mountain
countries: Canada
coordinates: lat: 57.715555555555554
lon: -130.63472222222222
With this annexation, the recreation area was greatly reduced in size to around. This remnant of the recreation area was east of Mount Edziza until 2003 when it was disestablished. 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: mount edziza
instance_of: Mountain
countries: Canada
coordinates: lat: 57.715555555555554
lon: -130.63472222222222
Basalt at Mount Edziza is in the form of alkali basalt and hawaiite; the latter is thought to be the product of partial fractional crystallization in subterranean magma chambers. Volcanic rocks of intermediate composition such as trachybasalt, tristanite, mugearite and benmoreite are restricted to Ice Peak where they form the upper part of this subsidiary peak.

Geographic entities mentioned:
surface_form: ice peak
instance_of: Mountain
countries: Canada
coordinates: lat: 57.6906
lon: -130.635
Indigenous peoples. Mount Edziza lies within the traditional territory of the Tahltan people which covers an area of more than. Historically, Mount Edziza and other volcanoes of the Mount Edziza volcanic complex were sources of obsidian for the Tahltan people.

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