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This concise overview explores essential concepts related to intrusive igneous structures, highlighting the significance of viscosity in magma behavior and volcanic activity. It addresses how pressure and time (measured in pascal-seconds) influence fluid dynamics, discusses the differences between viscous and pseudoviscous materials, and examines the buoyancy of magma versus surrounding rock. Moreover, it outlines how gas pressure contributes to volcanic eruptions and the effect of plate tectonics on magma movement. Case studies from various geological formations illustrate these principles.
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Viscosity • Units: pascal-seconds (kg/m-sec) • How many pascals pressure x how many seconds to squash fluid flat? • Viscous: Material flows as long as pressure is applied, however small • Pseudoviscous: Material flows after some threshold stress
What Drives Magma? • Magma is typically 10% lighter than equivalent solid rock • Why pressure inhibits melting • Buoyancy drives magma upward • Weight of rock around volcanic conduit > weight of magma • Gas pressure powers volcanic eruptions • Mafic (dense) rocks can sink in crust by viscous flow