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Dynamics of the Earth
 
I. Evidence of Crustal Motions: ,[object Object],Weathering & Erosion ( Uplift ) Plate tectonics
B. Sedimentary  beds are deposited as _______________ __(_____  _) Horizontal Layers Strata
THIS SEDIMENTARY STRATA  SHOWS NO EVIDENCE OF UPLIFT OR CRUSTAL MOTION LAW OF ORIGINAL HORIZONTALITY
C. Evidence of motions within the Earth’s crust is indicated by: 1._____________ 2._____________ 3._____________ Tilting Folding Faulting
TILTING
FOLDING
FAULTING: OFF SET LAYERS
FAULTING
 
D.  ______________ provide direct  evidence of crustal movement. Earthquakes
World Distribution
U.S . Distribution
_______  ______ and ________  _______  are 2 changes that can be observed after an earthquake. Fault  lines Uplifted  land  (displaced strata)
EARTHQUAKE DAMAGE
 
 
E. ______  ________ are used in mapping surveys and indicate exact positions and elevations. Bench  marks
Changes in ________________ of benchmarks are evidence that the land is either   ___________  or____________ rising sinking elevation
F.Displaced  marine  fossils  found in mountains have 2 interpretations: 1. _____________________________ _______________________________ 2. _____________________________ ________________________________ Higher sea levels  covered mountains Rocks were uplifted from a previous ocean bottom
G. _____________ is the rising  of the crust _____________  is the sinking  of the crust Uplift Subsidence
II: EARTHQUAKES
[object Object],[object Object],[object Object],A. 2 processes that cause earthquakes: magma volcanoes faulting
[object Object],[object Object],Slow stress
Increased pressure causes the _______  _______ to break creating a ________.  Rock  strata fault
When faulting occurs  energy radiates through  the earth as  _ _______  _ _______  that cause the ground to _______________ Seismic  waves vibrate
III.Measuring the Earthquakes: ,[object Object],[object Object],[object Object],Mercalli Richter
[object Object],[object Object],[object Object],[object Object],Mercalli intensity 1 12
Mercalli Scale  – Intensity scale I II III IV V VI
[object Object],[object Object],[object Object],[object Object],Richter Scale magnitude energy
[object Object],[object Object],1 10 31X
Richter Scale  – Magnitude scale
V. Parts of the Earthquake: ,[object Object],focus
 
[object Object],epicenter
A. The 2 most important energy waves are: ,[object Object],[object Object],[object Object]
P-wave Primary Wave S-wave Secondary wave
B. Characteristics of Primary Waves (P) waves: ,[object Object],[object Object],[object Object],[object Object],Faster than S waves Recorded first travels through both solids and fluids
C. Characteristics of Secondary Waves (S) waves: ,[object Object],[object Object],[object Object],[object Object],Slower than P waves Recorded after P-wave Can  not  travel  through fluids
TYPES OF EARTHQUAKE WAVES
[object Object],[object Object],denser
VI. Finding the Epicenter: ,[object Object],[object Object],magnitude Records arrival time  of seismic waves  Use reference table page 11
Seismograph
 
SF = San Francisco 300 km LV = Las Vegas 390 km LA = Los Angeles 189 km Seismic Stations TRIANGULATION TO FIND THE EPICENTER SF LV LA 300 km
Skip Page 4 in your out line! Start with VIII: The Layers of the Earth
VIII. THE LAYERS OF THE EARTH: ,[object Object],[object Object],[object Object],[object Object],varies thinner thicker
[object Object],[object Object],granitic dark dense basaltic low light
B. Inferred characteristics of Earth’s Interior: ,[object Object],[object Object],transmission Earth Quake Waves
S-waves can not pass through liquid
P-waves are bent as they pass through the different layers Based on the density of the layer
[object Object],[object Object],velocity density refracted
[object Object],[object Object],[object Object],[object Object],solid liquid gas solid
[object Object],[object Object],[object Object],[object Object],[object Object],S and P waves S P liquid
S-waves can not pass through liquid
[object Object],refraction interfaces
 
L et’s Draw This Diagram in our Notebook :

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