Earthquakes
... Displacement occurs along discrete segments 100 to 200 kilometers long Most segments slip every 100-200 years producing large earthquakes Some portions exhibit slow, gradual displacement known as fault creep ...
... Displacement occurs along discrete segments 100 to 200 kilometers long Most segments slip every 100-200 years producing large earthquakes Some portions exhibit slow, gradual displacement known as fault creep ...
Gravity - Lauren - s3.amazonaws.com
... Universal gravity is the force of gravity on every object to an extent. Example: The earth has a bigger gravitational pull on us, because the earth has a greater mass. We have a smaller mass compared to the earth, so our gravitational pull is smaller to the earth. Question: Does someone who is bigge ...
... Universal gravity is the force of gravity on every object to an extent. Example: The earth has a bigger gravitational pull on us, because the earth has a greater mass. We have a smaller mass compared to the earth, so our gravitational pull is smaller to the earth. Question: Does someone who is bigge ...
Homework_3_2009
... Natural Hazards - Geology 209 Homework assignment #4 - Earthquakes and Seismology Due Date: Feb. 17th ...
... Natural Hazards - Geology 209 Homework assignment #4 - Earthquakes and Seismology Due Date: Feb. 17th ...
Chapter 19: Earthquakes - Richmond County Schools
... of damage caused by a quake and is measured by the Modified Mercalli Scale – Uses roman numerals – Higher the number the greater the damage ...
... of damage caused by a quake and is measured by the Modified Mercalli Scale – Uses roman numerals – Higher the number the greater the damage ...
Physics 111 - Lecture 6 Dynamics, Newton’s Laws (Summary)
... Newton’s First Law of Motion Every body continues in a state of rest or uniform velocity unless it is compelled to change that state by a net force acting upon it. • Inertia of an object is its tendency to maintain its present state of motion. Mass is a measure of Inertia. Newton’s Second Law of Mot ...
... Newton’s First Law of Motion Every body continues in a state of rest or uniform velocity unless it is compelled to change that state by a net force acting upon it. • Inertia of an object is its tendency to maintain its present state of motion. Mass is a measure of Inertia. Newton’s Second Law of Mot ...
seismic waves
... • Seismic waves radiate out from the source in all directions. • Siesmograph stations recieve p and s waves and use the difference in arrival time to determine the distance away. • Different stations compare the information recorded at the same time. ...
... • Seismic waves radiate out from the source in all directions. • Siesmograph stations recieve p and s waves and use the difference in arrival time to determine the distance away. • Different stations compare the information recorded at the same time. ...
CH. 8 Pre-Test
... 11. The intensity of an earthquake is partially determined by the a. type of fault on which it occurs. c. amount of damage it causes. b. gap hypothesis. d. amount of ground motion. ...
... 11. The intensity of an earthquake is partially determined by the a. type of fault on which it occurs. c. amount of damage it causes. b. gap hypothesis. d. amount of ground motion. ...
Earthquakes - hrsbstaff.ednet.ns.ca
... – Parts of plates stick because of friction – As the rest of the plate continues to slide, more friction energy is created. ...
... – Parts of plates stick because of friction – As the rest of the plate continues to slide, more friction energy is created. ...
name________________________
... A. BLAMING SOMEONE ELSE FOR WHAT YOU DID B. THE MOVEMENTS OF ROCK ALONG A FAULT C. THE VIBRATION OF CRUST D. NONE OF THESE 15. IN REGARD TO WAVES, HERTZ IS THE SAME AS A. VELOCITY B. FREQUENCY 16. DRAW IN AND LABEL ALL FOUR BASIC LAYERS OF THE EARTH ...
... A. BLAMING SOMEONE ELSE FOR WHAT YOU DID B. THE MOVEMENTS OF ROCK ALONG A FAULT C. THE VIBRATION OF CRUST D. NONE OF THESE 15. IN REGARD TO WAVES, HERTZ IS THE SAME AS A. VELOCITY B. FREQUENCY 16. DRAW IN AND LABEL ALL FOUR BASIC LAYERS OF THE EARTH ...
Earthquakes
... (ii) Secondary (shear waves): 3.5 km/sec, particles move perpendicular to the direction of wave motion (Fig. 6) Longitudinal (surface waves): up and down + side to side movement; drag + shear!, slowest. Intensity of earthquakes Mercalli intensity scale Magnitude of earthquakes Richter's scale: For a ...
... (ii) Secondary (shear waves): 3.5 km/sec, particles move perpendicular to the direction of wave motion (Fig. 6) Longitudinal (surface waves): up and down + side to side movement; drag + shear!, slowest. Intensity of earthquakes Mercalli intensity scale Magnitude of earthquakes Richter's scale: For a ...
What are Earthquakes
... • Result of P-waves and S-waves when they reach the surface • Only travel in the crust! • Slowest seismic waves • Make the ground roll like ocean waves • Responsible for surface damage and falling buildings. ...
... • Result of P-waves and S-waves when they reach the surface • Only travel in the crust! • Slowest seismic waves • Make the ground roll like ocean waves • Responsible for surface damage and falling buildings. ...
Earth`s Waters Section 1–1 Review and Reinforce (p. 17) 1
... Section 2-3 Review and Reinforce (p. 57) 1. Earthquakes can damage or destroy buildings, bridges, and other structures, topple utility poles, fracture gas and water mains, and trigger landslides, avalanches, and tsunamis. 2. Seismic waves transfer energy from hard, dense rock to loosely packed soil ...
... Section 2-3 Review and Reinforce (p. 57) 1. Earthquakes can damage or destroy buildings, bridges, and other structures, topple utility poles, fracture gas and water mains, and trigger landslides, avalanches, and tsunamis. 2. Seismic waves transfer energy from hard, dense rock to loosely packed soil ...
