Which mechanism allows strike-slip motion on the Mendocino transform fault to cause localized uplift along segments?

💡 Explanation

When strike-slip motion occurs through fault bends or stepovers, compressional strain builds up locally because the plates are forced together rather than sliding freely, causing uplift. Therefore compressional strain results in uplift, rather than rebound, thermal expansion, or deposition which require different conditions.

• Which mechanism maintains persistent surface high-pressure zones around 30 degrees latitude?
• Which risk increases when porous alluvial aquifers are rapidly depleted by irrigation pumping?
• Which geological process commonly generates strike-slip faults in Earth's crust?
• Which pedogenic effect is accelerated when earthworm bioturbation increases?
• Which outcome occurs when stress exceeds static friction along an existing transform fault?
• Which mechanism leads to increased stream flooding in mountainous regions following extensive deforestation?