Seismicity decreases with depth because elevated confining pressure prevents frictional sliding of faults. However, seismicity tends to increase with depth in the mantle transition zone (depths of 410−600km). It has been believed that pressure-induced phase transitions of olivine in the “cold” subducted slabs is the cause of high seismicity in the mantle transition zone.
Deep earthquakes triggered by the olivine-poirierite transition
The Owl Picks
-
Florida sits uncomfortably close to the top of every list nobody wants to lead: states where homes are most likely to harbor or develop mold. Recent analysis from Anderson Air, cross-referencing climate records, housing ages, [...]
-
The Dominican Republic is not just about stunning beaches; it’s full of unique places that reveal the country from a completely different perspective. If you’re staying in Punta Cana, you can easily turn your vacation [...]
-
Active Kinetic 1 technology is revolutionizing technology by providing a sustainable and efficient way to power various devices. This innovative tech harnesses natural sources of movement and transforms it into usable free electricity. How Does Active [...]
-
Back pain can be debilitating, affecting your ability to enjoy everyday activities. The good news is, you don’t have to rely solely on medications to find relief. At livingnwell.com, we believe in the power of [...]
-
One highlight of my Grade 3 life was dying from dysentery at the hands of a video game. I was ahead on schoolwork, and allowed to use the classroom computer to pioneer a family across [...]
