17- Earthquake Hazard Flashcards
What causes earthquakes
Along a fault, large rock masses are moving past each other pushed by tectonic forces. When stress builds up to a critical point (10-100s of years), and the accumulated stress is greater than the friction forces, there is enough force to cause a sudden slip along the fault, releasing stored strain energy. This produces shock waves into surrounding rock.
Focus/ Hypocenter
Originating point of an earthquake on the fault line
Epicenter
Point on surface directly above focus
Body waves
Transmit energy through the earths interior in all directions from the earthquakes focus
Divided into:
P waves:
-travel through solids and liquids
-compressional wave, material pushed parallel to travel path
- ~5km/s
S-waves:
-travel only through solids
-up, down motion that pushed material at right angle to wave path
- ~2-3km/s
Surface waves
Transmit energy along earths surface, causing surface to vibrate.
Includes 2 waves: (both cause extensive damage to rigid structures)
Love waves:
-restricted to earths surface
-cause sideways shaking of the ground(think snake), causing extensive damage to rigid structures
-speed slightly less than s waves
Rayleigh waves:
-produce rolling motions of the ground (imagine water ripple)
-slightly lower velocity than S waves
How are earthquakes measured
- Intensity
- subjective measure based on damage and people’s reaction
-measured using modified mercalli intensity scale
-factors that affect intensity; distance from epicenter, focal depth, population density, local geology, duration and building types - Magnitude
- quantitative measure of energy released at its source using Richter scale
- base 10 logarithmic scale, converts largest recorded seismic wave to numerical magnitude
- each number increase = 10 fold increase in shaking amplitude and 30 fold increase in energy release
IMPORTANT: earthquake has single magnitude regardless of distance, but intensity differs with distance
Geology affect on earthquake intensity
Ground shaking: amplitude, duration and damage increases in poorly consolidated soil
Ex. Solid bedrock will inhibit large damage, thick soils will settle, increasing potential for damage(liquefaction)