Mapa mental
TOPIC 4: PHYSICS
Contenido del mapa
TOPIC 4: PHYSICS
ULTRASOUND
- SOUND WITH FREQUENCIES HIGHER THAN 20,000 Hz (20 kHz)
- ABOVE AND BEYOND THE HEARING RANGE OF HUMANS
- THE WAVES GET PARTIALLY REFLECTED AT A BOUNDARY BETWEEN MEDIA BECAUSE OF THE CHANGE IN DENSITY (PARTIAL REFLECTION)
- THE TIME IT TAKES FOR THER EFLECTION TO REACH THE DETECTOR CAN BE USED TO MEASURE HOW FAR AWAY THE BOUNDARY IS
- USES
- PRE-NATAL SCANNING OF A FOETUS ( SAFER THAN X-RAYS)
- SONAR USED BY BOATS TO DETECT OTHER BOATS, MARINE ANIMALS, THE SEA BED AND ROCKS
- SOUND WITH FREQUENCIES HIGHER THAN 20,000 Hz (20 kHz)
INFRASOUND
- SOUND WITH FREQUENCIES LESS THAN 20 Hz
- BELOW THE HEARING RANGE OF HUMAN
- USES
- USED BY ANIMALS TO COMMUNICATE ( ELEPHANTS, BATS, TIGERS) THEY CAN DIFFRACT AROUND OBJECTS EASILY( LONG DISTANCES)
- PRODUCED BY METEOR STRIKES AND VOLCANIC ERUPTIONS
- SOUND WITH FREQUENCIES LESS THAN 20 Hz
THE EARTHS STRUCTURE
- CRUST
- MANTLE
- OUTER CORE
- INNER CORE
- SOLID AND IS THOUGHT OF TO BE MADE OF IRON AND NICKEL
- LIQUID
- INNER CORE
- HAS PROPERTIES OF A SOLID EXCEPT THAT IT CAN FLOW VERY SLOWLY. RADIOACTIVE DECAY OCCURS IN THE MANTLE
- OUTER CORE
- WE LIVE ON IT BUT IT'S VERY THIN (ABOUT 20KM)
- MANTLE
- MADE UP OF TECTONIC PLATES
- THEY FLOAT ON TOP OF THE MANTLE AND MOVE A FEW CM PER YEAR
- AT PLATE BOUNDARIES THE PLATES MAY SLIDE PAST EACH OTHER WHICH SOMETIMES CAUSES EARTHQUAKES
- THEY ARE VERY HARD TO PREDICT
- AT PLATE BOUNDARIES THE PLATES MAY SLIDE PAST EACH OTHER WHICH SOMETIMES CAUSES EARTHQUAKES
- THEY FLOAT ON TOP OF THE MANTLE AND MOVE A FEW CM PER YEAR
- CRUST
SEISMIC WAVES
- CAUSED BY EARTHQUAKES AND EXPLOSIONS
- WE DETECT THESE WAVES ALL OVER THE SURFACE OF THE EARTH USING SEISMOMETERS
- 2 TYPES
- P-WAVES
- THEY ARE LONGITUDINAL, FASTER THAN S-WAVES AND CAN TRAVEL THROUGH LIQUIDS AND SOLIDS
- S-WAVES
- THEY ARE TRANSVERSE ARE SLOWER THAN P-WAVES AND CAN ONLT TRAVEL THROUGH SOLIDS
- P-WAVES
- REFLECT AND REFRACT AT BOUNDARIES BECAUSE OF THE DIFFERENT LAYER IN THE EARTH ( DIFFERENT DENSITIES)
- SEISMOMETER RESULTS (SEISMOGRAMS)
- YOU CAN WORK OUT THE EPICENTRE ( CENTRE OF THE EARTHQUAKE)
- ON THE READINGS YOU CAN TELL WHICH IS THE P-WAVE AND S-WAVE ASTHE P-WAVE IS THE QUICKEST AND WILL ARRIVE FIRST
- TRIANGULATION IS USED TO DETECT WHERE THE EARTHQUAKE'S EPICENTRE
- ON THE READINGS YOU CAN TELL WHICH IS THE P-WAVE AND S-WAVE ASTHE P-WAVE IS THE QUICKEST AND WILL ARRIVE FIRST
- YOU CAN WORK OUT THE EPICENTRE ( CENTRE OF THE EARTHQUAKE)
- CAUSED BY EARTHQUAKES AND EXPLOSIONS
Información
- Descripción
- Mapa Mental sobre TOPIC 4: PHYSICS, creado por durber.katie el 01/06/2013.
- Creado por
- durber.katie
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