Chap 17 Flashcards
Geophysics
The study of seismic waves and earths magentic field gravity and heat
Oceanic crust
-7m thick
Layer one: marine sediment
Layer 2: pillow basalt overlying basaltic dikes
Layer 3: Sill like gabbro intrusions
Seismic reflection
The return of some waves to the surface after bouncing off a rock layer boundry
Seismic refraction
Bending of seismic waves as they pass from one material to another having different seismic waves velocities
Seismic waves
indiciate crust is thinner and denser beneath the oceans than on the continents
Lithosphere
Crust and uppermost mantle 70 km thick beneath oceans, 125 km thick beneath continents
Moho
boundary between crust and mantle
Asthenosphere
beneath lithosphere partially molten rock low velocity zone
Isostasy
Equilibrium of adjacent blocks of brittle “floating on upper mantle
Isostatic adjustment
Rising or sinking of crustal blocks to achieve isostatic balance
Crustal rebound
Rising of crust after large mass of ice was rapidly remoced from the surface at the end of ice ages
Gravitational force
Determined by the mass and the distance between objects
Positive gravity anomaly
gravity reading higher than normal indicate that tectonic forces hold up a region out of isostatic equilibrium
Negative gravity anomoaly
gravity reading lower than normal
Magnetic field
region of magnetic force
North and south magnetic poles