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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
 
B. The steps for calculating your distance from the epicenter: ,[object Object],[object Object],[object Object],[object Object],Subtract arrival time of  P from arrival time of S Mark the interval on Y-axis Slide marks to match P & S curve Follow down to x-axis and read distance
01:10:00 01:20:00 01:18:00 01:24:00
Step 1 ,[object Object],[object Object],[object Object],[object Object],[object Object],[object Object]
Step 2 ,[object Object]
Step 3 ,[object Object],[object Object]
Step 4 ,[object Object]
 
Practice questions: ,[object Object],[object Object],[object Object],4 minutes 2600 Km
Practice questions: ,[object Object],[object Object],[object Object],[object Object],[object Object],3 minutes 1800 Km
Practice questions: ,[object Object],[object Object],[object Object],[object Object],[object Object],1500 Km
Practice questions: ,[object Object],4 minutes
Practice questions: ,[object Object],[object Object],6 mins 40 secs
VII. THE ORIGIN TIME OF AN EARTHQUAKE: ,[object Object],later greater
B. To find the origin time seismologists need to know: ,[object Object],[object Object],Arrival time of P-wave Travel time of P-wave (how long it took)
Example: ,[object Object],[object Object],[object Object]
[object Object],[object Object],[object Object],[object Object],The answer is:  9 min . 2:36
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
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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Earthquake Notes Slide show

Hinweis der Redaktion

  1. Start here on Monday Period 3!!!! We left off discussing this chart and it’s meaning on Page 11 of the Earth Science reference tables.
  2. Stop here and give class work for double period.
  3. Use the demo that Mr. Mckee make