Earth quakes-Science Flashcards
Stress:
Force that acts on rock to change its shape or volume.
Three types of stress:
Tension, compression, shearing
Volume:
The amount of space a rock takes up.
Tension:
Stretches rock, crust gets thinner in the middle.
Compression:
Squeezes rock, rock folds or breaks.
Shearing:
Pushes dock in two different directions, rock slips or changes shape.
Fault:
A break in Earth’s crust.
Strike-slip fault:
There is little up or down motion.
Normal fault:
The hanging wall slips downward below the footwall.
Reverse fault:
The hanging wall slides up and over the footwall.
True or false? A strike-slip fault that forms the boundary between two plates is called a convergent boundary.
False, convergent boundary, no, it’s a transform boundary.
Hanging wall:
Slips downward when movement occurs along a normal fault. It occurs when the fault is at an angle. Above fault line.
Normal faults and Reverse faults:
The faults are at an angle. The faults have footwalls.
Shearing: Type of fault: Type of movement:
Type of fault: strike-slip Type of movement: horizontal
Tension: Type of fault: Type of movement:
Type of fault: Normal Type of movement: vertical
Compression: Type of fault: Type of movement:
Type of fault: reverse Type of movement: vertical
Which 2 types of faults result in mountains? How do you know?
Normal and Reverse, they move up
Anticline:
Arch, fold in rock that bends upward.
Syncline:
Sinks in, file in rocks that bends downward.
Folded mountains:
Whole thing, parallel ridges and valleys.
How is a fault-block mountain created?
It is created by two normal faults.
Plateau:
Tall, flat area. A large flat area of land higher then the area around it.
Type of fault:
Stress force:
Movement along fault:
Fault: Reverse fault
Stress force: compression, Movement along fault: vertical
Fault: Normal fault
Stress force: tension
Movement along fault: vertical
Fault: Strike-slip fault
Stress force: shearing
Movement along fault: horizontal