pp. 738-746 chapter 21 section 2 earthquakes & volcanoes
TRANSCRIPT
P P. 7 3 8 - 7 4 6
Chapter 21 Section 2Earthquakes & Volcanoes
EARTHQUAKES
• Occur due to plate movement faults
• Introduction to Earthquakes• It’s an Earthquake Song
EARTHQUAKES: FOCUS VS. EPICENTER
• Focus: point UNDER Earth’s surface where waves originate…along the fault line
• Epicenter: point ON Earth’s surface directly above the focus…surface waves begin here and move outward• Focus of an Earthquake
SEISMIC WAVES
•3 types of seismic waves:1.P-waves2.S-waves3.Surface waves
Seismic Waves Song
P-WAVES
• P (primary)-waves: move the fastest• Rocks are squeezed & pushed in direction of
wave (longitudinal)• P-Wave Animation
S-WAVES
• S (secondary/shear)-waves: rocks move at right angles (transverse) to direction of waves
• Slower than P-waves• S-Wave Animation
SURFACE WAVES
• Rocks move sideways and up & down• Slowest of the three types of waves• Most destructive wave
Surface Wave Animation
HOW ARE EARTHQUAKES MEASURED?
• Seismograph: instrument that can detect, amplify, and record ground vibrations too small to be perceived by human beings
• Seisomogram: a graph showing the motion of the ground versus time
• Seismograph Animation• Seismograph-ing to the beat• Cali Seismogram Real Time
TRAVEL-TIME CURVES
• Measures the time between P & S-waves (that hit a particular seismic station)• Wave speed differs b/c of
density & rigidity of Earth’s layers
• Tells you the distance of location from epicenter
• As the time between waves increases the distance from epicenter increases• Time & Distance= Direct
relationship!
LOCATING THE EPICENTER
• Use travel-time curve
• Ex. Difference between P & S waves=6.3 min• What’s the distance
from the epicenter?• 4,000 km
BIG DEAL? WHAT DOES THAT TELL US…
• By looking at travel-times of seismic waves to different stations, we can generate a probability of epicenter location (scale distance on map)
• See circles around d1, d2 and d3?
• Where all 3 circles intersect tells us epicenter!
• Quake Movie Trailer
DETERMINING DESTRUCTION• Richter Scale
– measures magnitude (energy of largest seismic wave) on 1-10 scale– looking at the wave’s largest
amplitude
– Each magnitude is 10 times stronger than the previous magnitude
– Ex: magnitude 8 earthquake releases as much energy as detonating 6 million tons of TNT!• Japan March 2011 Tsunami Photos
Nat. Geo.• Tsunami Animation• Largest EQs Since 1900
DETERMINING DESTRUCTION CON’T
• Modified Mercalli Scale• amount of shaking experienced at
different locations (intensitydamage)
• Varies based on:• overall magnitude• how far you are from the fault that
ruptured in the earthquake• rock/ land texture or type (i.e. sand vs.
concrete)
• More meaningful measure of severity to the nonscientist because intensity refers to the effects actually experienced at that place.
VOLCANOES
Mt. St. Helens
ZONES OF VOLCANISM• Volcanism: all the processes associated with the release of
magma, hot fluids, and gas• Fueled by magma
• Rises to surface because less dense • Called lava once at surface
LOCATION OF VOLCANOESNOT RANDOM!
• Mostly determined by plate boundaries• Most at convergent and divergent boundaries• 5% far from boundaries
MAJOR BELT OF CONVERGENT VOLCANOESCircum-Pacific Belt
(Pacific Ring of Fire)– Outlines the
Pacific Plate – Convergent
volcanism:– Plates colliding– Continental
subduction zones
– Characterized by explosive eruptions
DIVERGENT VOLCANISM
• Formed where plates move apart• New ocean floor is produced here• Pillow lava forms at ocean ridges• Characterized by non-explosive eruptions• About 2/3 of Earth’s volcanoes occur at divergent
boundaries• Ex: Icelandic volcanoes uncharacteristically explosive due to hot spot
HOT SPOTS• Unusually hot regions of Earth’s mantle where high-
temperature plumes (columns) of magma rise to the surface
• Usually form far from plate boundaries• Stationary – plate moves over spot
• Ex: Hawaiian Islands
Bend in chain change in direction of plate
movement!
VOLCANO ANATOMY
• Conduit: tube-like structure that magma travels through to surface
• Vent: opening that lava comes out of
• Crater: bowl-shaped depression around the vent – Usually less than 1 km (0.6 mi) in diameter
TYPES OF VOLCANOES• Appearance determined by:• Type of
material that forms volcano
• Type of eruptions
• 3 types:1. Shield2. Cinder cone3. Composite
1.
2.
3.
SHIELD VOLCANOES
• Broad, gently sloping sides• Non-explosive, quiet eruptions• Made of layers of basaltic lava• Largest type (width wise)
• Ex: Mauna Loa (Hawaii)
CINDER CONE
• Steep sides, cone shaped• Mostly basaltic lava• Explosive eruptions • Smallest type (most less than 500 m or 0.3 mi high)• Often on or near larger volcanoes
• Ex: Lassen Volcanic Park (California)
• Large, cone shaped, concave slopes• Much larger than cinder cones
• Made of layers of rock (harden lava) from explosion and lava flows
• Violent eruptions (with periods of quiet ones)• Ex: Mt, Augustine (Alaska), Mt. St. Helens
(Washington)
COMPOSITE VOLCANO
MT. VESUVIUS, ITALY • Catastrophic eruption of A.D. 79 destroyed the
cities of Pompeii and Herculaneum and killed at least 16,000 people
• Buried 10’ deep with lava & ash• Thermal energy570 degrees F (300 degrees C)
• most died instantly of extreme heat, with many casualties shocked into a sort of instant rigor mortis.
• Most died instantly of extreme heat, with many casualties shocked into a sort of instant rigor mortis.