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Holocene volcanism

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Snake River Plain
valley in Idaho, United States
Haruj
Haruj (, also known as Haroudj) is a large volcanic field spread across in central Libya. It is one of several volcanic fields in Libya along with Tibesti, and its origin has been attributed to the effects of geologic lineaments in the crust.
Elmenteita Badlands
mountain in Kenya
Azas Plateau
volcanic field in Russia
Volcanic Eifel
region in the Eifel Mountains in Germany, that is defined to a large extent by its volcanic geological history
Indian Heaven
mountain in United States of America
Cascade Volcanoes
chain of volcanoes in western North America
Udokan Plateau
volcano
Yellowstone hotspot
hotspot
2007–2008 Nazko earthquakes
series of earthquakes in Canada
Mount Cayley volcanic field
mountain in Canada
Garibaldi Volcanic Belt
volcanic chain in British Columbia, Canada
Meidob Volcanic Field
mountain in Sudan
Khanuy-Gol
300px|thumb|Uran-Togoo Khanuy-Gol (also known as Bulgan Volcanic Field, Chanuj Gol Hanui Gol or Hanuy Gol) is a volcanic field in Mongolia. Khanuy-Gol is located in the northern Hangai range, north of the settlement of Bulgan. 300px|thumb|Topographic map It covers a surface area of southwest of Ulaanbaatar. Among the 10 cones with heights of that make up the field are Baga Togo Uul/Bogo-Togo-Ula (meaning "Little Togo Mountain", high, to ), Ikh Togo Uul/Ikha-Togo-Ula (meaning "Great Togo mountain", high, ), Togo, Urun Dush, and Uran Uul. This cone is the highest of the field, with a height of
San Francisco Volcanic Field
geologic feature in Arizona, United States
Northern Cordilleran Volcanic Province
Geologic province primarily located in British Columbia and Yukon, Canada.
Big Raven Plateau
plateau in British Columbia, Canada
Laguna Mariñaqui
mountain in Chile
Itasy Volcanic Field
volcanic field in Madagascar
Apastepeque
volcanic field
Anahim Volcanic Belt
linear belt of volcanoes
Bayuda Volcanic Field
volcanic field in Sudan
Bus-Obo
Bus-Obo is a high cinder cone in Mongolia. The high cone is formed by basaltic rocks. It may be of Pleistocene or Holocene age.