Which mechanism primarily causes uplift in fault-block mountain ranges resulting from normal faulting?

💡 Explanation

When a normal fault occurs, one block slides downward relative to the other, causing isostatic rebound because the removal of overlying material reduces lithospheric loading, initiating buoyant uplift. Therefore buoyant isostatic forces causes uplift, rather than compressional folding, differential erosion, or simple crustal thinning alone.

• Which geologic consequence directly follows the continued glacial erosion within a cirque?
• Which mechanism influences stream course alignment in areas bisected by a transform fault?
• Which outcome typically occurs on the leeward side of a volcanic island in steady trade wind conditions?
• Which mechanism causes increased stream discharge variability in regions transitioning from glacial to fluvial drainage patterns?
• Which feedback loop affects thermohaline circulation when Arctic ice melt introduces freshwater into the North Atlantic?
• Which topographic outcome results when aeolian deflation dominates?