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...as '''Iskut River Cone''', is a [[cinder cone]] of the [[Iskut-Unuk River Cones]] group in northwestern [[British Columbia]], [[Canada]], located on the st [[Category:Cinder cones of British Columbia]] ...

| name = Cinder Cone | photo = Cinder Cone.jpg ...

...ound is part of the Big Lava Bed, a 0.9 cu km lava flow erupted from the [[cinder cone]] in the background about 8200 years ago. The [[lava flow]] traveled 1 | type = [[Fissure vent]], [[cinder cone]] and [[lava field]]<ref name="SI"/><ref>{{cite gvp|name=Indian Heaven ...

[[Category:Cinder cones of British Columbia]] [[Category:Polygenetic volcanoes]] ...

...sky ] at Aster Voɭcano Archive JPL NASA</ref> Their lava flows and cinder cones have dammed a valley dissecting the mountain, creating the Bolshoye Goltsov [[Category:Polygenetic shield volcanoes]] ...

...[[Chilcotin Plateau]]. The volcanic field contains at least eight volcanic cones and is one of two volcanic fields in the [[Anahim Volcanic Belt]], the othe | - || [[Cinder cone]] || - || - || {{nowrap|{{Coord|52|44|N|124|33.8|W|type:mountain_regio ...

...e caldera contain numerous very youthful basaltic-to-andesitic pyroclastic cones and lava flows. ...uary 2016|language=es}}</ref> Holocene activity may have formed the cinder cones on the northeastern side of the caldera.<ref>{{cite book|chapter=Seismic an ...

...on. Wells Gray Tours, Kamloops, BC. {{ISBN|978-0-9681932-3-5}}.</ref> Both cones were built upon unweathered glacial material.<ref>{{cite book|last1=Dashtga ...t is breached on its north side by a lava flow from a flank eruption. Both cones comprise unconsolidated irregular [[volcanic block]]s with little agglutina ...

| type = [[Cinder cone]]s ...ng first appeared in April 1850. It consists of a gravelly [[basalt]]ic [[cinder cone]], which contrasts greatly with the surrounding verdant hillsides, and ...

* [[Cinnamon Butte]], a volcanic field, [[lava dome]]s, and [[cinder cone]]s * [[Wizard Island]], a cinder cone and volcanic [[island]] ...

...ns (1789 and after) are confined within and around an active polygenetic [[cinder cone]] in a {{Convert|2|km|mi|abbr=on}} wide [[caldera]] that was formed by [[Category:Polygenetic cinder cones]] ...

...[[shield volcano]]es; these shields are topped by small spatter and cinder cones, and the field includes a number of [[subglacial volcano]]es and [[tuya]]s. ...st 700,000 years. The last volcanic activity in the field produced a large cinder cone, [[Big Lava Bed]], as well as a voluminous [[lava]] and [[scoria]] flo ...

...lcano's flanks. Most of them are [[cinder cone]]s and [[Cinder cone|scoria cones]], but there are also some [[lava dome]]s and about 20 [[tuff ring]]s near [[Category:Polygenetic shield volcanoes]] ...

...es, including outstanding examples of [[Volcanic cone#Spatter cone|spatter cones]].{{sfn|Kiver|Harris|1999|p=340}} The 60 distinct solidified lava flows tha [[File:Rafted parts of North Crater.jpeg|thumb|left|Cinder crags from North Crater on the North Crater Flow]] ...

...495-9 }}</ref> Over 100 [[cinder cone|cinder]] and [[volcanic cone|spatter cones]] are arranged along these rift zones. Hualālai has no [[caldera|summit ca |[[Volcanic vents|Vent]] [[Scoria|cinder]] deposits with black [[pahoehoe]] basalt [[lava]] flows formed during AD [ ...

...h|2006|p=206}} On the western and southwestern side of the complex, some [[cinder cone]]s can be found,{{sfn|Richards|Ullrich|Kerrich|2006|p=203}} and [[fiss ...nsist of [[cinder cone]]s and lava flows with small volumes. Some of these cones are partially eroded,{{sfn|Kraemer|Adelmann|Alten|Schnurr|1999|p=171}} othe ...