3.1. Hazardous environments resulting from tectonic movement Flashcards
1
Q
Define earthquakes
A
- the shaking/trembing caused by the sudden release of energy
- usually associated with faulting/breaking of rocks
- continuing adjustments of position results in aftershocsk
2
Q
Define focus/hypocenter
A
The point within the earth where faulting begins
3
Q
Define epicentre
A
The point directly above the focus on the surface
4
Q
Why do earthquakes occur?
A
- Occur along plate margins
- Plates move at a rate between 1.5cm and 7.5cm per year
- When plates move past/towards/away from each other, the movement is not smooth as friction causes the plate to get stuck => causes pressure to build up
- Energy waves then race rapidly from the focus causing commotion on the ground
5
Q
Elastic Rebound Theory
A
Explains how energy is stored in rocks:
- Rocks bend until the strength of the rock is exceeded
- Rupture occurs and the rocks quickly rebound to an undeformed shape
- Energy is released in waves that radiate outward from the fault
6
Q
2 types of body waves (wave that travel within earth’s interior)
A
- P Wave/Pressure wave/Primary wave
- S wave/Sheer wave/Secondary wave
7
Q
P Waves
A
- The fastest body waves
- These are compressional waves where the material movement is in the same direction as wave movement
- They travel through solids and liquids
8
Q
S Waves
A
- Slower than P-waves
- Travel with a sideway motion and move material perpendicular to wave movement thus making the ground move horizontally
- Travel through solids only
- Cause a lot of damage
9
Q
Mohorovicic Discontinuity - Moho
A
- Seismographs close to epicentre showed slow travelling P-waves and S-waves which contrasted with the faster moving P-waves and S-waes further away from the shock
- If the shock waves pass through the denser rocks, they speed up and vice versa
- S-waves don’t go through solid so stop at outer core
- Whereas, P-waves are refracted
10
Q
Types of seismic waves/surface waves (travels through crust)
A
- Slower than body waves
- Long/love waves (cause ground to move sideways)
- Rayleigh waves (cause ground to move up and down
11
Q
Impact of P-waves
A
Can turn solid sediments into fluids like quicksand by disrupting sub-surface water conditions. This is known as liquefaction or fluidisation
12
Q
Different types of fault
A
- Normal dip-slip faults: results from tension in crustal rocks pulling apart
- Reverse dip-slip faults: results from compression in the crust collision
- Strike-slip faults: results from crustal blocks sliding past each other
13
Q
Richter scale
A
- Measures magnitude of a tremor using seismometer which records data on seismograph
- Logarithmic scale (a size 2 s 10 times larger than 1)
- Less than 3: not felt
- 3-3.9: felt, little damage
- 4-4.9: some structural damage
- 5-5.9: losses in populated areas
- 6-6.9: large losses in urban area
- 7-7.9: serious building damage, major loss of life
- >8: total destruction
14
Q
Mercalli scale
A
- measures how much damage is caused by the earthquake based on observations (a result of surface shaking)
- measures intensity of earthquake by indicating the violence of the earth motion
- scale between 1 and 12
15
Q
Differences between Richter and Mercalli
A
- Richter measures strengths, Mercalli measures damage/effects
- Richter scale is based on scientific data, Mercalli is based on people’s observations
- Richter measured by seismometers, Mercalli measured by people
- Mercalli uses whole number, Richter uses numbers to one decimal place