火山锥

火山锥（英语：volcanic cone）是最简单的火山地形之一。它们是由火山喷口的喷射物建置的，在喷口周围堆积成带有中央火山口的圆锥体形状。火山锥有不同的类型，取决于喷发过程中喷射出的碎片的性质和大小。火山锥的种类包括层锥(stratocone)、飞溅锥(spatter cone)、凝灰岩锥(tuff cone)、和火山渣锥^[1]^[2]。

参见

火山渣锥

参考资料

^ Poldervaart, A. Volcanicity and forms of extrusive bodies. Green, J; Short, NM (编). Volcanic Landforms and Surface Features: A Photographic Atlas and Glossary. New York: Springer-Verlag. 1971: 1–18. ISBN 978364265152-6.
^ Schmincke, H.-U. Volcanism. Berlin, Germany: Springer-Verlag. 2004. ISBN 978-3540436508.

[Poldervaart1971a-1] Poldervaart, A. Volcanicity and forms of extrusive bodies. Green, J; Short, NM (编). Volcanic Landforms and Surface Features: A Photographic Atlas and Glossary. New York: Springer-Verlag. 1971: 1–18. ISBN 978364265152-6.

[Schmincke2004a-2] Schmincke, H.-U. Volcanism. Berlin, Germany: Springer-Verlag. 2004. ISBN 978-3540436508.

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