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Many excellent images can be found on Wikimedia Commons, especially in the categories listed at right. Note that many images which are available on Commons are not properly categorized yet, so it is helpful to also search directly for images there. Thousands of other useful free images can be found on the websites listed below.
{{Portal:Volcanoes/Selected picture/Layout |image=Image.jpg |size=size in pixels (if applies) |caption=rollover text |text=image description |link=link to the volcano's/volcanic feature's article }} Please make sure that the picture is relevant to volcanism and is not related to any of those already featured (for example, two pictures of Mt. Fuji).
Mount Hasan (Turkish: Hasan Dağı) is a volcano in Anatolia, Turkey.It has two summits, the 3,069 metres (10,069 ft) high eastern Small Hasan Dagi and the 3,253 metres (10,673 ft) high Big Hasan Dagi, and rises about 1 kilometre (0.62 mi) above the surrounding terrain.
The three common popular classifications of volcanoes can be subjective and some volcanoes thought to have been extinct have erupted again. To help prevent people from falsely believing they are not at risk when living on or near a volcano, countries have adopted new classifications to describe the various levels and stages of volcanic activity ...
Shishaldin Volcano, or Mount Shishaldin (/ ʃ ɪ ˈ ʃ æ l d ən /), is one of six active volcanoes on Unimak Island in the eastern Aleutian Islands of Alaska. [1] It is the highest mountain peak of the Aleutian Islands, rising to a height of 9,373 ft (2,857 m) above sea level.
This is a list of active, dormant, and extinct volcanoes located beyond planet Earth. They may be designated mons (mountain), patera (an irregular crater) or tholus (small mountain or hill) in accordance with the International Astronomical Union's rules for planetary nomenclature. Many of them are nameless.
They can happen on land as well, where rising magma that comes into contact with an aquifer (water-bearing rock formation) at shallow levels under the volcano can cause them. [50] The products of Surtseyan eruptions are generally oxidized palagonite basalts (though andesitic eruptions do occur, albeit rarely), and like Strombolian eruptions ...
A lack of extant erosion shows that Mount Cleveland is likely a Holocene volcano, forming within the last 10,000 years. [9] All known events have occurred at Mount Cleveland's summit vent, [4] but there are at least five small andesite to dacite volcanic domes on the lower flanks. [14] At times Cleveland has had a summit lava dome.
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