Earthquakes: rapid motion or trembling of the ground when rocks in the Earth’s interior break or slide past each other due to sudden, unexpected release of stored elastic energy in the rocks
Focus/Hypocenter: site along the rupturing fault where earthquakes and waves originate
Epicenter: position of the Earth’s surface directly above the focus
Depth: distance between focus and the earth’s surface
Seismic Waves: vibrations caused by moving rocks
Body Waves: transverse through the earth’s interior; faster and higher frequency
Surface Waves: transverse only through the earth’s surface; responsible for most of an earthquake’s damage
Seismograph: equipment to record/measure how strong an earthquake is
Igneous rocks: formed from hardened magma and lava
Sedimentary rocks: particles of other rocks that have been weathered and eroded
Metamorphic rocks: undergo changes due to heat and pressure
Weathering: is a term for all processes which combine to cause the disintegration and chemical alteration of rocks at or near earth's surface.
Erosion: includes all the processes of loosening, removal, and transportation which tend to wear away the earth’s surface.
Lithification is the conversion of unconsolidated sediment into solid rock.
Primary Waves (P waves): faster and compressional/longitudinal (motion of particles is parallel to the direction of the wave); can move in solids and liquids
Secondary Waves (S waves): longitudinal wave, stretched and compressed
Uniformitarianism: the processes that shaped the earth
Divergent are where the plates move away from each other
Convergent where the plates move tears each other
Transform: slides past each other
Plate tectonics: the earth’s crust is broken into plates which can move