Term
| Earth’s interior is made up of |
|
Definition
| Silicon, Oxygen, Iron, and Magnesium |
|
|
Term
|
Definition
outer part of earth which is rocky; it is thinner at the ocean than at continents. |
|
|
Term
|
Definition
| boundary about 40 km below surface, 7 km on ocean floor |
|
|
Term
|
Definition
| the crust and upper mantle it floats on the Asthenosphere |
|
|
Term
|
Definition
| near top of; mantle, high temp. and pressure causes small melting of rock. – Less dense rock rises and others sink |
|
|
Term
| 2 parts of the core and contents |
|
Definition
| outer is liquid, probably made of iron, responsible for magnetic field. Inner is sold, iron and nickel |
|
|
Term
|
Definition
| liquid, solids, and gases form cells, bring new rock to crust. Evidence suggest entire continent drift on convection |
|
|
Term
|
Definition
| Area where plates stick together as they try to move pressure builds and earthquakes occur |
|
|
Term
|
Definition
source of earthquake waves travel in all directions below surface |
|
|
Term
|
Definition
|
|
Term
|
Definition
| primary waves) fast moving longitudinal waves. 1rst to reach equipment. Also, it can travel through any material |
|
|
Term
|
Definition
| (Secondary waves) slow moving transverse waves. They move side to side, through solids only |
|
|
Term
|
Definition
| (L waves) – interaction of p and s waves, cause surface to shake and roll, worst destruction |
|
|
Term
|
Definition
| area in Earth not affected by P and S waves because of density of material |
|
|
Term
|
Definition
| instrument used to record earthquakes need S location to locate epicenter |
|
|
Term
|
Definition
| size and magnitude of earthquakes measures amount of energy released |
|
|
Term
|
Definition
| hypothesized continents were once joined together called Pangaea |
|
|
Term
|
Definition
| in crust through which magma reaches Earth’s surface |
|
|
Term
|
Definition
| edge of Pacific Ocean lots of volcanoes and earthquakes |
|
|
Term
|
Definition
| bend in rock caused by force |
|
|
Term
|
Definition
- process of mountain building (orogenic belts) – Rock mountains
|
|
|
Term
|
Definition
large areas lifted without breaking rocks |
|
|
Term
|
Definition
|
|
Term
|
Definition
|
|
Term
|
Definition
| angle at which rock layer is tilted from horizontal |
|
|
Term
|
Definition
| forms a straight line from dip |
|
|
Term
|
Definition
| occurs when force is great enough to break rock and not fold. – no movement along facture is called a joint |
|
|
Term
|
Definition
| area where crust is spreading. – in middle of Atlantic ocean, molten rock from mantle rises through rifts or cracks in ocean floor. – Forms mid – Atlantic Ridge. Also on land as the Great Rift Valley in Africa |
|
|
Term
|
Definition
| when plates press together. Produces mountains, volcanoes, and ocean trenches. Marianna trench |
|
|
Term
|
Definition
| where one plate is forced under another. Oceanic plate under continental plate forming a trench. Marianna trench is 11,000 m deep, greatest depth reached |
|
|
Term
|
Definition
| when 2 plates slide past each other in opposite directions. Ex. San Andreas fault |
|
|
Term
|
Definition
| form along a fracture where there is movement |
|
|
Term
|
Definition
Earth’s crust is pulled apart known as tension. As the crust moves and tilts form Fault Block Mountains |
|
|
Term
|
Definition
| when the crust is pushed together known as compression. (Thrust fault) – angle is very low |
|
|
Term
|
Definition
| crust drags against each other in opposite directions known as shear. Hanging wall and footwall move parallel to each other. Ex. San Andreas. |
|
|