Which outcome is amplified when colliding tectonic plates experience increased mantle convection?

💡 Explanation

Increased mantle convection enhances upward magma flow, fueling subduction zone volcanism via decompression melting, because the increased flow rate overcomes prior impedance. Therefore eruptions become more powerful, rather than accretion/isostasy which are surface processes independent of magma source rates.

• Which consequence results when prolonged drought increases wind velocity and sediment looseness in a semi-arid landscape?
• Which consequence results when unimpeded longshore drift encounters a dredged navigation channel?
• Which outcome occurs when viscous magma continually erupts, forming an unstable lava dome?
• Which outcome occurs when an increased rate destabilizes thermoclines?
• Which lakebed formation results when wind-driven deflation lowers the surface near the water table?
• Which outcome develops when intense tropical rainfall alters surface soil profiles?