Channel: ParrMr

Category: Education

Tags: charlie puthtensionnormal faultfocusstrike slipreverse faultp waves wavegoing onshearingmr. parrsurface waveepicenterhow longcompressionparrmrearthquake waves

Description: Going On (Earthquake Waves) Pushing it’s compression What happens? It fold ‘til Rock is made to spread and break apart Like some gum from tension, pulling the rock tight, but Opposite sides cut, shearing involved See dead down in the crust so deep Focus where the rock lets go, yeah Instead, surface seismograph sees Epicenter, waves will show The waves like this keep going on Like accordion they’re P When they’re side to side, S be The waves like this keep going on When they’re up and down, shaky Combined surface waves they be, crazy A strike slip is a fault Side to side it’s moving Normal pulling away they’re apart Collide, they collide, reverse fault you see that Making mountains pulling the crust up, ooh yeah See dead down in the crust so deep Focus where the rock lets go, yeah Instead, surface seismograph sees Epicenter, waves will show The waves like this keep going on Like accordion they’re P When they’re side to side, S be The waves like this keep going on When they’re up and down, shaky Combined surface waves they be, crazy The waves like this keep going on baby Through solid rock is how See dead down in the crust so deep Focus where the rock lets go, yeah Instead, surface seismograph sees Epicenter, waves will show The waves like this keep going on… Like accordion they’re P When they’re side to side, S be The waves like this keep going on When they’re up and down, shaky Combined surface waves they be, crazy The waves like this keep going on When they’re up and down, shaky The waves like this keep going on, baby The waves like this keep going on When they’re up and down, shaky Combined surface waves they be, shaky