Presentation on theme: "By Andrea Snell Revised by GBrenneman S and How they shape the Earth."— Presentation transcript:
By Andrea Snell Revised by GBrenneman S and How they shape the Earth
Earthquakes are a sudden movement of Earth’s crust that releases energy. CA quake (clip) Text pgs. 54-58CA quake ▪ The crust of the Earth is constantly moving, but are usually slow – until a major earthquake takes place. ▪ About 95% of all earthquakes occur at or near the edge of moving plates. Worldwide Earthquake LocatorWorldwide Earthquake Locator ▪ They occur along cracks in the Earth’s crust called faults. Faults are associated with, or form, the boundaries between Earth’s tectonic plates. ▪ Earthquakes do not occur randomly.
How do earthquakes workHow do earthquakes work ?
Types of stress in the Earth’s crust lead to fault lines.stress
Types of Faults Strike-slip faults Normal Faults Reverse Faults
Modeling Fault Types Animations of fault types Animations of fault types ▪ Foam Fault Models and Examples Foam Fault Models and Examples
Normal Faults (Tension) Normal Faults create space. Two pieces of the crust pull apart, spreading the crust apart.
Reverse Faults (Compression) Reverse faults squeeze the crust and push two blocks of crust on top of one another. Usually these faults are found in the Rocky Mountains and Himalayas and cause mountains to form.
Strike-slip Faults (Shearing) Indicates rocks are sliding past each other, with little to no vertical movement. Both the San Andreas and Anatolian Faults are strike-slip.
Epicenter and Focus (text pgs. 64-77) video lecture video lecture The epicenter is the point the Earth’s surface, or land, directly above the earthquake focus. The focus is the hypocenter of an earthquake. The vibrating waves travel away from the focus of the earthquake and move in all directions. Earthquakes do not start at the epicenter.
Earthquake Waves The energy from an earthquake travels away from the focus in waves. The waves travel in different speeds. There are two types of waves 1. Those that travel inside the Earth 2. Those that travel only at the surface
Waves that travel inside the Earth Demo of S waves and P waves Demo of S waves and P waves Primary Waves, or P Wave, are “push-pull” waves that cause back-and- forth vibrations in the same direction as the waves move. The P-Waves are fast-moving. Secondary Waves, or S waves, cause vibrations at right angles to the waves direction of travel. The S waves are slow- moving.
Surface Waves Surface waves explanation Surface waves explanation Surface waves- only travel only at the surface and move slower than P-waves or S-waves. These waves make the ground roll and sway. They can cause a great deal of damage to buildings, roads, and other surface features. pool shakespool shakes
Locating an Earthquake Lab DEMO (see teacher for lab sheet and tools) Finding the epicenter using triangulation example Finding the epicenter using triangulation example
Measuring Earthquakes Earthquakes are recorded by instruments called seismographs. Seismographs record seismic waves. The motion is measured electronically and recorded in a computer. They can measure both S and P waves. The size of the waves is called magnitude. To tell the strength of the earthquake scientists use a Richter Scale. The larger the number on the Richter Scale, the larger the earthquake. You won’t even feel an earthquake if it is below a 3. Today scientists also use the Moment-Magnitude scale. NASA sci file Each number is 32 times greater than the previous number. 4.0 -Would shake your house like a large truck passes by. 5.0 – Things might fall off shelves. Walls might crack and windows break. 7.0 – Weaker buildings could collapse. Also cracks may occur in streets. 8.0 – Buildings and bridges could fall down and large cracks in surface. 9.0 and up- Large scale damage and cities flattened.
Testing Buildings for Earthquake-Proofing ▪ Testing Testing
Japan’s Mega Earthquake Japan's Mega EarthquakeJapan's Mega Earthquake (48 mins.)
Tsunamis can be caused by earthquakes ▪ Japan's tsunami and how it happened (documentary) Japan's tsunami and how it happened (documentary)
How to Protect Yourself during an Earthquake Text pg. 77 ▪ Protect Yourself (interactive game) Protect Yourself ▪ Animation of how to stay safe Animation of how to stay safe
Landforms created by Earth’s stresses Part Two (text pgs. 58-61)
MOUNTAIN BUILDING How Tall Can a Mountain Be? How Tall Can a Mountain Be?
Fault-block Mountains ▪ Blocks drop down or lift up or tilt ▪ Occur along fault lines ▪ Sierra Nevada range
Mountain Building Demonstration Demonstration ▪ mountain building (clip) mountain building Fault-Block Mountains: When normal faults uplift a block of rock, a fault-block mountain forms. The Grand Tetons in Wyoming and Idaho are one such example. Mountain Building Types (clip)Mountain Building Types
Folded Mountains ▪ Formed when plates collide ▪ Rock crumples and folds ▪ Appalachians, Himalayas
More mountains Folds are compressions from two plates colliding. The Appalachian Mountains were formed in this way.
Anticlines and Synclines Anticlines and Synclines can be found in folded mountains. Anticlines, such as the Black Hills in South Dakota, are the folds in the rock that bend upward while synclines, such as the Illinois Basin, are the folds in the rock that bend downward.
Volcanic Mountains ▪ Form from layers of volcanic material ▪ Cascades in Oregon and Washington
Dome Mountains ▪ A form of folded mountain ▪ Just one fold bumps up in the middle ▪ Adirondacks in New York
Plateau - a large area of flat land elevated high above sea level How the Grand Canyon Was Formed How the Grand Canyon Was Formed
Summarizer ▪ Mountain Building Types of Mountains Mountain Building Types of Mountains ▪ Fault Lines IN America Fault Lines IN America ▪ Demonstration of Mountain Building Demonstration of Mountain Building ▪ Faults and Folds – Modeling Faults and Folds – Modeling ▪ Faults Model Faults Model
Science is so Cool! ▪ earthquake exhibit earthquake exhibit ▪ Hands-ON Fun ▪ Make It Quakeproof (add link)