Article · Wikipedia archive · Last revised Jul 18, 2026

Volcano-sedimentary sequence

A volcano-sedimentary sequence is a stratigraphic succession composed of interbedded volcanic, sedimentary, and volcaniclastic rocks, formed through the contemporaneous or alternating activity of volcanic processes and sedimentary deposition, commonly in tectonically active settings such as rifts or volcanic arcs. These successions typically include lava flows, pyroclastic deposits, sedimentary structures, and reworked volcaniclastic material, reflecting the coupled interaction between volcanism, erosion, transport, and sedimentation within evolving basins.

Last revised
Jul 18, 2026
Read time
≈ 1 min
Length
93 w
Citations
1
Source

A volcano-sedimentary sequence is a stratigraphic succession composed of interbedded volcanic, sedimentary, and volcaniclastic rocks, formed through the contemporaneous or alternating activity of volcanic processes and sedimentary deposition, commonly in tectonically active settings such as rifts or volcanic arcs. These successions typically include lava flows, pyroclastic deposits, sedimentary structures, and reworked volcaniclastic material, reflecting the coupled interaction between volcanism, erosion, transport, and sedimentation within evolving basins.1

References

References