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The structure and emplacement of cinder cone fields. An overview by Richard Fletcher
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Study objectives Identifying differences in emplacement and structures between flank cinder cones and flat lying volcanic field cones. Flank cones studied around: Mauna Kea. Hawaii; Mt. Etna, Italy; Kilimanjaro, Tanzania. Platform cones studied around: San Francisco Mtn., Arizona; Paricutin region, Mexico; Nunivak Island, Alaska.
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Overview of Climatic conditions and ages of cones
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Primary Study Areas
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Implications Lunar cones have smaller rim heights and larger basal diameters due to less gravity and atmospheric drag. Morphometeric analysis suggests the shape and size is a function of age and erosive processes. Younger cones indicate active volcanism methods (conduits and dikes).
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