Which risk increases along strike-slip faults connecting seafloor spreading centers?

💡 Explanation

High stress accumulates in the transform fault zone because lateral motion resists friction via elastic deformation and brittle failure. Therefore, there is a greater risk of intense earthquake occurrences, rather than diffuse volcanism or ice formation, which involve different geological processes.

• Which process exacerbates desertification when ephemeral streams deposit sediment on alluvial fans?
• Which erosional pattern emerges when acidic groundwater percolation weakens cave structures?
• Which feedback mechanism explains higher sea surface temperatures that disrupt upwelling within an ocean gyre?
• Which consequence results when coastal upwelling ceases near a major fishing ground?
• Which risk increases when constructing structural foundations on sloping alluvial deposits?
• Which consequence frequently results when heavy tephra accumulates downwind?