Relatively thin compared to the crust below the continents
Continentalcrust
Made up of lighter, less dense granite rocks
Mantle
A layer of rock materials between the crust and the core
Mohorovicicdiscontinuity or Moho
Marks the boundary between the crust and the mantle
Discontinuity
The interphase of two layers, marked by the sudden change of density of the rock layers
Core
Located at the Earth's center
Layers of the core
Inner core
Outer core
Inner core
Believed to be made up of solid iron, responsible for Earth's magnetic field
Outer core
Thought to be composed of liquid iron-nickel alloy due to extremely high temperature
The deepest hole drilled only went 13km deep
Continental Drift Theory
Theory by Alfred Wegener that the world's continents were once part of a single landmass called Pangaea
Pangaea likely began to split around 200 million years ago, and have continued to move to where they are now
Plate Tectonic Theory
Earth's solid, brittle lithosphere is broken into several tectonic plates that glide over the partially molten asthenosphere
Boundary
The place where two plates meet
Types of plate boundaries
Divergent
Transform
Subduction or Convergent
Divergent Boundary
Formed between two plates that are moving away from each other
Transform Boundary
Also called conservative plate boundaries, formed between two plates that are moving horizontally past each other
The San Andreas is the most popular transform boundary
Convergent Boundary
Formed where two plates converge
Earthquake
The shaking of the ground due to the sudden movement of Earth's lithospheric plates
Types of earthquakes
Tectonic earthquake
Volcanic earthquake
Focus
The point underneath the epicenter where the displacement of rocks originated
Epicenter
The point on the surface of Earth directly above where the displacement of rocks originated
Fault
Zones of fracture where large blocks of rocks move relative to each other
Types of faults
Normal fault
Strike-slip fault
Reverse fault
Main earthquake zones
Circum-Pacific Belt
Alpide Belt
Mid-Atlantic Ridge
Circum-Pacific Belt
Also called the Ring of Fire due to the large number of active volcanoes
Alpide Belt
Extends from Java to Sumatra, through the Himalayas, the Middle East, the Mediterranean, and out into the Atlantic
Mid-AtlanticRidge
Consists mostly of an underwater mountain range
Intensity of an earthquake
Measure of the damage incurred on the surface and its perceived effects
RichterScale
Measures the magnitude of earthquakes
Instruments used to detect earthquakes
Seismograph
Laser rangefinder
Geiger counter
Extensometer
An earthquake can cause excessive damage to properties in towns and cities, including building and structure collapse, cracks and gaps in the ground, landslides, and tsunamis
What to do before, during, and after an earthquake
1. Before: Prepare emergency plans and supplies
2. During: Stay calm, take cover, avoid falling objects, move to higher ground if near water
3. After: Check for damage, assist others, make repairs
Magma
The molten rock that collects in compartments also known as magma chambers
Caldera
When volcanoes deplete the magma within their chambers, the volcano may collapse on itself, creating a large, basin-shaped volcanic opening