The volume of product released in any one eruption can vary enormously indigenous a couple of cubic metres of magma to as much as 3,000 cubic km (720 cubic miles). A series of tiny eruptions commonly builds up mounds close to the vent, vice versa, large-volume eruptions tend to disperse their products over a better distance. Effusive eruptions kind lava plateaus or gently sloping shield volcanoes; moderately explosive eruptions type stratovolcanoes; and also giant explosive eruptions kind plateaus the lava or ash flows and nearly always type a caldera numerous kilometres in diameter end the eruption site. Naturally, because many other factors are affiliated in determining volcano landforms, there space exceptions to this rules.

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Lava flowing toward the sea from Kilauea volcano, Hawaii, takes 2 recognizable forms: fast-flowing, ropy lava, called pahoehoe, and thick, blocky lava, called aa.

The chemical composition of magma influence its physics properties, i beg your pardon in turn have actually a major influence ~ above the landform developed by a volcanic eruption. Four common volcanic rock varieties are detailed in the table: basalt, andesite, dacite, and also rhyolite. As the silica contents increases, these rock types generally become much more viscous; together the magmatic gas content increases, lock become an ext explosive. Other physical nature are, however, necessary in identify the character of lava flows. Because that example, warm basaltic lava produces flows with smooth come ropy surfaces. This flows, recognized as pahoehoe, tend to circulation farther than the cooler aa flows of the same chemical composition that have rough, damaged surfaces. (See the section Lava flows.)

If a volcano has consistent eruption habits, that is landform will reflect that character. The form of the large but gently sloping shield volcano Mauna Loa, for example, indicates a long record of eruption of fluid lava flows, when the beautiful, symmetrical shape of the stratovolcano mount Fuji indicates a lengthy record of center explosive eruptions indigenous its summit the produce alternate layers the ash and lava. In comparison to straightforward shield and stratovolcanoes, many volcanoes change their eruptive habits—both in eruption form and in the ar of their vents—over time. This results in a mixture of volcanic landforms called a facility volcano.

The geometry the the vent or vents likewise exerts profound regulate on volcano landforms. Many point-source vents that erupt only once or at most a few times form a volcanic field of dozens of tiny cinder cones quite than a single large volcanic edifice. Volcanic vents in the kind of lengthy fissures usually build up a special lava plateau (especially once erupting voluminous quantities of fluid lava) or a low volcanic mound. Hekla Volcano in Iceland is transitional in between plateau-building fissure eruptions and eruptions indigenous a single major vent that create a symmetry stratovolcano. Hekla erupts native a fissure the is parallel come the Mid-Atlantic Ridge and around 20 kilometres (12 miles) in length. Perceived along the fissure, Hekla looks prefer a stratovolcano; perpendicular come the fissure, it shows up as an elongate ridge.

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Finally, however of great importance, is the atmosphere where the volcanic products are erupted—into the atmosphere, under water, or under ice. Submarine volcanoes space surprisingly comparable to your counterparts top top land, but their slopes are generally steeper because water cools the lavas an ext rapidly. Deep submarine volcanism often tends to be much less explosive due to the fact that the push of the water retards explosive boiling. Subglacial volcanism produces landforms that space dramatically different from those produced by subaerial volcanism. This is particularly apparent in Iceland, wherein glaciers covered the whole island 15,000 year ago, and big ice caps quiet cover extensive locations today. Fissure eruptions in ~ the ice type steep ridges of broken lava fragments rather than lava-flow plateaus, while subglacial eruptions native point-source vents that erupt repeatedly form table mountains. Table hill volcanoes have actually steep sides of pillow lavas—sacklike structures that kind when flows of basaltic lava are extruded into the ocean, a deep lake, or a water-filled cavern within ice. These pillow structures space capped by number of tens the metres of broken lava pieces from explosive shallow-water eruptions. The broken lava pieces in turn are overlain through shield-building lava operation erupted over the glacial surface.