![]() ![]() The lavas of stratovolcanoes are higher in silica, and therefore much more viscous, than lavas from shield volcanoes. Classic examples include Mount Fuji in Japan, Mayon Volcano in the Philippines, and Mount Vesuvius and Stromboli in Italy.Īsh produced by the explosive eruption of stratovolcanoes has historically posed the greatest volcanic hazard to civilizations. They are also known as composite volcanoes because they are created from multiple structures during different kinds of eruptions. Stratovolcanoes (composite volcanoes) are tall conical mountains composed of lava flows and tephra in alternate layers, the strata that gives rise to the name. Stratovolcanoes (composite volcanoes) Cross-section through a stratovolcano (vertical scale is exaggerated): In New Mexico, Caja del Rio is a volcanic field of over 60 cinder cones.īased on satellite images, it was suggested that cinder cones might occur on other terrestrial bodies in the Solar system too on the surface of Mars and the Moon. Parícutin in Mexico and Sunset Crater in Arizona are examples of cinder cones. Cinder cones may form as flank vents on larger volcanoes, or occur on their own. These can be relatively short-lived eruptions that produce a cone-shaped hill perhaps 30 to 400 meters (100 to 1,300 ft) high. Izalco erupted almost continuously from 1770 (when it formed) to 1958, earning it the nickname of "Lighthouse of the Pacific".Ĭinder cones result from eruptions of mostly small pieces of scoria and pyroclastics (both resemble cinders, hence the name of this volcano type) that build up around the vent. Main articles: volcanic cone and Cinder cone Izalco volcano, the youngest volcano in El Salvador. Active mud volcanoes tend to involve temperatures much lower than those of igneous volcanoes except when the mud volcano is actually a vent of an igneous volcano. Other types of volcano include cryovolcanoes (or ice volcanoes), particularly on some moons of Jupiter, Saturn, and Neptune and mud volcanoes, which are formations often not associated with known magmatic activity. ![]() Vents that issue volcanic material (including lava and ash) and gases (mainly steam and magmatic gases) can develop anywhere on the landform and may give rise to smaller cones such as Puʻu ʻŌʻō on a flank of Kīlauea in Hawaii. Some volcanoes have rugged peaks formed by lava domes rather than a summit crater while others have landscape features such as massive plateaus. The features of volcanoes are much more complicated and their structure and behavior depends on a number of factors. The most common perception of a volcano is of a conical mountain, spewing lava and poisonous gases from a crater at its summit however, this describes just one of the many types of volcano. Skjaldbreiður, a shield volcano whose name means "broad shield" Plate tectonicsįurther information: Types of volcanoes Lakagigar fissure vent in Iceland, the source of the major world climate alteration of 1783–84, has a chain of volcanic cones along its length. The study of volcanoes is called volcanology, sometimes spelled vulcanology. The word volcano is derived from the name of Vulcano, a volcanic island in the Aeolian Islands of Italy whose name in turn comes from Vulcan, the god of fire in Roman mythology. For example, Mercury has pyroclastic deposits formed by explosive volcanic activity. Other planets besides Earth have volcanoes. Historically, large volcanic eruptions have been followed by volcanic winters which have caused catastrophic famines. Large eruptions can affect atmospheric temperature as ash and droplets of sulfuric acid obscure the Sun and cool the Earth's troposphere. Volcanoes are usually not created where two tectonic plates slide past one another. This results in hotspot volcanism, of which the Hawaiian hotspot is an example. Volcanism away from plate boundaries has been postulated to arise from upwelling diapirs from the core–mantle boundary, 3,000 kilometers (1,900 mi) deep in the Earth. Volcanoes can also form where there is stretching and thinning of the crust's plates, such as in the East African Rift and the Wells Gray-Clearwater volcanic field and Rio Grande rift in North America. For example, a mid-ocean ridge, such as the Mid-Atlantic Ridge, has volcanoes caused by divergent tectonic plates whereas the Pacific Ring of Fire has volcanoes caused by convergent tectonic plates. On Earth, volcanoes are most often found where tectonic plates are diverging or converging, and most are found underwater. For broader coverage of this topic, see Volcanism.Ī volcano is a rupture in the crust of a planetary-mass object, such as Earth, that allows hot lava, volcanic ash, and gases to escape from a magma chamber below the surface. ![]()
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