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Boundaries converge subduction, descension divergent margins widen convective from the core red hot and sticky hardening to obsidian succumb to subterranean pull an infinitesimal slide below dense and pressured soil the slow parting seam a rift becomes a chasm consuming solid ground
0
Nov 10, 2016
Nov 10, 2016 at 11:54 AM UTC
Tectonic
Boundaries converge subduction, descension divergent margins widen convective from the core red hot and sticky hardening to obsidian succumb to subterranean pull an infinitesimal slide below dense and pressured soil the slow parting seam a rift becomes a chasm consuming solid ground
denel-kessler
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Nov 10, 2016
Nov 10, 2016 at 11:54 AM UTC
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