Defects & Earthquakes Flashcards
3 causes of defects in rock masses
- tectonic forces (compression, shear, tension)
- uplift and/or erosion
- cooling of lava = contraction
2 forms of defect
joints (no movement parallel to fracture surface) and faults (movement parallel to the fracture surface)
define a joint
defect that exhibits little or no movement parallel to the plane of fracture
joint sets
parallel joints within a rock mass
columnar jointing
as lava cools it contracts, cools from outside inwards forming a polygonal joint network. longer cooling = wider columns
joint spacing vs. aperture
joint spacing is the size of an individual block, whereas aperture is the distance between adjacent walls.
joint persisitance
length into the rock
joint lining
implies water flow
infilling of joints
can enhance strength e.g. quartz veining
how do joints affect permeability of rock?
increase permeability, movement of water controlled more by fractures than porosity
faults definition
generally planar fractures that exhibit displacement parallel to fracture plane
Normal faults (DIP-SLIP)
- occur in response to extensional tectonic forces
________ is a wall you can walk on. ________ wall is an overhead and ______ is the ammount of vertical displacement, with ______ being the horizontal displacement.
footwall is a wall you can walk on. _hanging _ wall is an overhead and throw is the ammount of vertical displacement, with heave being the horizontal displacement.
how does the hanging wall move in relation to the footwall in normal vs. reverse fault?
hanging wall moves down with respect to footwall in a normal fault. opposite in reverse fault
reverse faults (DIP-SLIP)
occur in response to compressional tectonic forces
heave vs heave ho
heave ho compressional and related to reverse fault
thrust faults
low angle (less than 15 degrees) reverse fault
strike-slip faults
response to shearing tectonic forces. No vertical movement e.g alpine fault in the south island