Zusammenfassung der Ressource
Waves & the Earth
- P1.18 Infrasound
- frequencies
- humans hear between 20Hz-20,000Hz
- infrasound - below 20Hz
- uses
- communication between animals
- e.g. whales&elephants
- detecting animal movement in remote location
- detecting volcanoes&meteors
- calculations
- P1.19 Ultrasound
- frequencies
- ultrasound - above 20,000Hz
- uses
- sonar
- find depth of water below boat
- communication between animals
- e.g. bats&dolphins
- foetal scanning
- calculations
- P1.20 Seismic Waves
- P&S waves
- caused by earthquakes+explosions
- P waves=longitudinal
- faster
- travel through liquids+solids
- S waves=transverse
- slower
- travel through solids
- detected by seismometres
- reflection&refraction
- seismic waves reflected&refracted
- at boundaries between crust,mantle+core
- P1.22 Detecting Earthquakes
- hard to predict when
- unsure of size of forces acting on tectonic plates
- unsure of amount of friction on plates
- locating earthquakes
- 1. many seismometers detect P&S waves
- 2. P=faster so arrives first
- greater difference in time between waves=greater difference between seismometer+earthquake
- 3. scientists work out distance from each seismometer
- find out where earthquake happened
- at least 3 seismometers used
- causes of earthquakes
- 1. tectonic plates move due to convection currents in mantle
- 2. plates slide past each other
- 3. friction-don't slide smoothly
- 4. forces build up till part of plate breaks
- 5. plates move with sudden jerk-earthquake!