16) Describe and sketch the shape of the following volcanoes. Identify the differences in eruptive materials. A) Cinder cones B) Shield volcanoes C) Composite/stratovolcanoes
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The Deep Dive
Cinder cones are the smallest type of volcanoes, resembling an inverted traffic cone with steep sides. They are formed by the explosive eruption of tephra, which consists of small ash and rock fragments that fall back to the ground around the vent, creating a symmetrical cone shape. These eruptions tend to be short-lived and primarily produce basaltic lava, resulting in relatively simple structures. Shield volcanoes, on the other hand, are broad and gently sloping with a shape reminiscent of a warrior’s shield lying on the ground. They erupt primarily low-viscosity basaltic lava, which can flow over large distances, contributing to their wide form. The eruptions are often non-explosive, forming layers of lava over time and creating massive structures like Mauna Loa in Hawaii. Composite or stratovolcanoes are tall, steep-sided mountains formed from a mixture of explosive eruptions and lava flows. They typically have a conical shape and are made from alternating layers of lava and volcanic ash, which contribute to their complex structure. These volcanoes often erupt andesitic or rhyolitic lava, which is more viscous and can cause explosive eruptions, such as those seen at Mount St. Helens or Mount Fuji.