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Earthqukes
Science
| Term | Definition |
|---|---|
| Earhquake | The shaking and trembling that results from the movement of rock beneath the Earth's surface. |
| Crust | The outer layer of the earth. |
| fault | Cracks in the tectonic plates. |
| mantle | The portion of the earth between the crust and the core. |
| lithosphere | The solid portion of the earth. |
| lithospheric plate | The dozen plates that make up the Earth's surface. |
| Seismoligists | a scientist who studies earthquakes. |
| S-Wave | A transverse earthquake wave that moves from side to side. |
| P-wave | A longitudinal earthquake wave that bounces up and down. |
| Surface Wave | A seismic wave that travels along or parallel to the earths surface. |
| Focus | The point of origin of an earthquake. |
| Epicenter | A point directly above the true center of disturbance,from which the shock waves of an earthquake apparently radiate. |
| Seismic Waves | A wave of energy that is generated by an earthquake or other earth vibrations that travel within the earth or along its surface. |
| magnitude | A measure of the size of an earthquake based on the quantity of energy released. |
| Tsunami | An unusually large sea wave produced by a seaquake or undersea volcanic eruption. |
| Liquefaction | The process by which sediment that is very wet starts to behave like a liquid. |
| aftershock | A small earthquake or tremor after a major earthquake. |
| Base Isolators | A pad that isolates a building from its foundation and prevents some of the earthquakes energy from entering the building. |
| Shear Core Walls | Transfers some of the earthquakes energy from roofs and floors to the building foundation. |
| Cross Bracing | Placed between stories to stiffen a buildings frame and absorb energy during an earthquake. |
| Mass Dampers | Absorb some of the energy from seismic waves |
| Flexible Piping | Bend as energy pass through them, greatly reducing earthquake damage. |
| Tension Ties | Devices firmly tied the floors and ceilings of a building to the wall.They absorb and scatter earthquake energy and thus reduce damage. |
| Stress | The force that acts on rock to change its shape or volume. |
| Tension | A type of Stress that stretches rock so that it becomes thinner in the middle. |
| Compression | A type of Stress that squeezes rock until it folds or breaks. |
| Strike-Slip Fault | A type of fault where rocks on either side move each other sideways with little up or down motion. |
| Normal Fault | A type of fault where the hanging wall slides downward caused by tension in the crust. |
| Reverse Fault | A type of fault where the hanging wall slides upward caused by compression in the crust. |
| Anticlyne | An upward fold in rock formed by compression in the earths crust. |
| Syncline | A downward fold of stratified rock in which strata slope towards a vertical axis. |
| Plateau | A large area of flat forces in the Earths crust push up a large flat block of rock. |
| Hanging Wall | a mass of rock overhanging a fault plane. |
| Foot Wall | a mass of rock hanging beneath a fault plane. |
| Shearing | a distinct motion of two rock surfaces against each other. |
| Richter Scale | a scale from 1 to 10 for indicating the intensity of an earthquake. |
| Mercalli Scale | A 12 point scale for expressing the intensity of an earthquake ranging from 1 to 12. |
| inner core | a solid sphere in the middle of the fluid core such as the iron-nickel core of the earth. |
| outer core | The outer side of a core |
| Basalt | A dark colored rock |
| Granite | A light colored rock |
| Continental Crust | A type of the crust |
| Oceanic Crust | A type of Crust |
| Divergent boundary | |
| Convergent boundary | |
| Transform boundary |