Jump to navigation Jump to search. Volcano Eruption Diagram. Explosive eruptions – magma is torn apart as it rises and reaches the surface in pieces known as pyroclasts. Effusive eruptions – magma rises through the surface and flows out of the volcano as a viscous liquid called lava. Answer geographically –tell me why there are many Volcanoes there. Flood basalts are the result of a giant volcanic eruption or series of eruptions that coats large stretches of land or the ocean floor with basalt lava. The type of eruption depends on the magma’s chemical composition and on the gas content, which affects the viscosity of magma (ability to flow). Another older name is trap basalt. a volcanic eruptions along rift fault zones that can flood large area with basalt flows. However, these are thought to be effusive eruptions producing fluid basalt lava rather than explosive eruptions producing ejecta. Eruption(s) at the Paraná and Etendeka traps igneous province had an eruptive volume of over 2.6 million cubic kilometers. Volcanic eruptions vary widely in strength. On the one extreme there are effusive Hawaiian eruptions, which are characterized by lava fountains and fluid lava flows, which are … a) Drawing an annotated diagram showing an explosivevolcano (Remember you will need to know why it is an explosive and not an effusive eruption and show that bit in your diagram) b) Explain why the Ring of Fire is given that name. Hawaiian eruptions are the calmest types of volcanic events characterized by the effusive eruption of very fluid basalt type lavas with low gaseous content. This category has the following 2 subcategories, out of 2 total. This eruption is displayed in the above diagram. Subcategories. Category:Diagrams of effusive eruptions. Effusive eruptions – magma rises through the surface and flows out of the volcano as a viscous liquid called lava. Effusive eruptions, meanwhile, are characterized by the outpouring of lava without significant explosive eruption. diagram showing the inside of a volcano eschooltoday the diagram representation above shows what a basic volcano looks like the magma chamber this is the area with massive collection of magma below the earth’s crust from which magma flows out crater after an eruption the tip or top of the volcano tends to blown off leaving a small depression at the top of it … Volcano - Volcano - Six types of eruptions: Volcanoes are frequently classified by their size and shape (as is described in the section Volcanic landforms), but they can also be classified by their eruptive habits. The two main different eruptive styles are, most simply put, explosive and effusive. From Wikimedia Commons, the free media repository. Students learn about the underlying factors that can contribute to Plinian eruptions (which eject large amounts of pumice, gas and volcanic ash, and can result in significant death and destruction in the surrounding environment), versus more gentle, effusive eruptions. D Diagrams of hawaiian eruptions (3 F) Diagrams of lava flows (14 F) Fluctuations between effusive and explosive behaviour during the course of eruptions can be entirely modulated by stress changes caused by the eruption, for … From wikimedia commons the free media repository. Explosive eruptions – magma is torn apart as it rises and reaches the surface in pieces known as pyroclasts. The Paraná and Etendeka eruption(s) occurred about 128 to 138 million years ago. Diagrams with french texts the request was initially asked to the french graphic lab. Geographically –tell me why there are many Volcanoes there to 138 million years ago effusive and explosive behaviour during course... 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