
Isometric illustration of volcano structure vector concept banner for web design Cross-section ofa volcano. Helens is an example of a composite cone volcano. Diagram of volcano isolated on white background stages of volcano infographic vector Volcano structure concept banner. The result is a cone that has a gentler slope than a cinder cone but is steeper than a shield volcano. Alternating eruptions of volcanic ash and lava cause layers to form. They form when different types of eruptions deposit different materials around the sides of a volcano. Composite cone volcanoes are also called stratovolcanoes. Hawaii’s Mauna Loa is a famous example of a shield cone volcano.Ī third type of volcanic cone is a composite cone. The lava spreads in a thin layer before cooling. The lava that erupts from these volcanoes is a thin liquid that slowly emerges from the center of the volcano as well as from cracks in its sides.

In contrast, shield volcanoes are characterized by a large, broad cone with sides sloping gently away from the center. Vesuvius is a famous cinder cone volcano. Its elevation is 4,169 m above sea level. Mauna Loa rises from the surrounding flat sea floor, and its diameter is in the order of 200 km. As a result, cinder cone volcanoes tend to be smaller than other types of volcanoes. The sizes and shapes of typical shield, composite, and cinder-cone volcanoes are compared in Figure 4.9, although, to be fair, Mauna Loa is the largest shield volcano on Earth all others are smaller. This type of eruption contains little lava, as the magma hardens and breaks into pieces during the explosion. Cinder cones form from ash and magma cinders-partly-burned, solid pieces of magma, that fall to the ground following a volcanic eruption. The steepest cones form around cinder cone volcanos. Volcanic cones can be steep or gently sloping depending on the type of eruption that forms them. CC BY 4.0 Figure 7.3.8 Hotspot Cross-Sectional Diagram by J. Have students check on the real-time status of some of the volcanoes tracked by the USGS by going to the provided online Volcano Status Map.A volcanic cone is a hill-shaped landform that forms around a volcano. Figure 7.3.1 Profiles of a Shield Volcano (Mauna Loa and Kilauea).
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Find out about different types of volcano, how to measure their strength and preparing. Have students add any new information to their worksheets. CCEA Volcanoes Volcanoes form when magma reaches the Earth's surface, causing eruptions of lava and ash.

Show students the National Geographic video “Volcanoes 101,” which profiles two of the most common volcano types-with Vesuvius and Kilauea as examples.ģ.

Encourage them to pay attention to descriptive phrases about the volcanoes. Tell students they will have an opportunity to check their information when they watch a video.Įxplain to students that they will watch a short video about two types of volcanoes. If students already know any information about the two types of volcanoes, enourage them to write it. Ask students to write the following labels: Ash Volcanic ash consists of rock, mineral, and volcanic glass fragments smaller than a tenth of an inch in diameteror slightly larger than a pinhead. Distribute a copy of the worksheet Venn Diagram to each student.
