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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

Ask by Fowler Sanders. in the United States
Dec 19,2024

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Cinder cones are steep, conical volcanoes made of cinders and ash, with explosive eruptions. Shield volcanoes have broad, gently sloping sides from fluid lava flows, resulting in non-explosive eruptions. Composite volcanoes, or stratovolcanoes, have layered structures with steep sides and can have highly explosive eruptions due to their mixture of lava and pyroclastic materials.

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To describe and sketch the shapes of the three types of volcanoes—cinder cones, shield volcanoes, and composite (stratovolcanoes)—let's break down each type, including their characteristics and differences in eruptive materials. ### A) Cinder Cones **Description:** - Cinder cone volcanoes are the simplest type of volcano. - They are formed from the accumulation of volcanic debris, primarily cinders, ash, and small volcanic rocks ejected during explosive eruptions. - The shape is typically conical with steep sides, and they usually have a bowl-shaped crater at the summit. **Eruptive Materials:** - Primarily composed of small fragments of lava (cinders) that solidify and fall back to the ground. - Eruptions are usually short-lived and can be quite explosive. **Sketch:** ``` /\ / \ / \ / \ / \ /__________\ ``` ### B) Shield Volcanoes **Description:** - Shield volcanoes have broad, gently sloping sides and are shaped like a warrior's shield. - They are formed by the eruption of low-viscosity basaltic lava that can flow over great distances. - These volcanoes typically have a wide base and a less steep profile compared to cinder cones. **Eruptive Materials:** - Composed mainly of fluid basaltic lava flows. - Eruptions are generally non-explosive and can last for long periods. **Sketch:** ``` ______ / \ / \ / \ / \ / \ /________________\ ``` ### C) Composite/Stratovolcanoes **Description:** - Composite volcanoes, also known as stratovolcanoes, have a layered structure formed from alternating eruptions of lava flows, ash, and other volcanic debris. - They typically have steep, conical shapes and are characterized by a central vent or crater. - These volcanoes are often associated with more explosive eruptions. **Eruptive Materials:** - Composed of a mixture of lava flows (which can be andesitic to rhyolitic) and pyroclastic materials (ash, pumice, and volcanic rocks). - Eruptions can be highly explosive due to the higher viscosity of the lava. **Sketch:** ``` /\ / \ / \ / \ / \ / \ /____________\ ``` ### Summary of Differences in Eruptive Materials: - **Cinder Cones:** Primarily cinders and ash; explosive eruptions. - **Shield Volcanoes:** Fluid basaltic lava; non-explosive eruptions. - **Composite/Stratovolcanoes:** Alternating layers of lava and pyroclastic materials; can be highly explosive. These sketches and descriptions provide a clear understanding of the shapes and eruptive materials associated with each type of volcano.

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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.

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