INTERIOR OF EARTH Flashcards
MAGNETISM OF EARTH IS CAUSED BY?
CONVECTIONAL CURRENTS IN OUTER CORE.
EPICENTER
ON THE SURFACE
HYPOCENTRE
INSIDE THE EARTH
P WAVES
LONGITUDINAL (COMPRESSIONAL/PRESSURE WAVES)
CAN TRAVEL IN ALL MEDIUM
S WAVES
TRANSVERSE (SHEAR/ DISTORTIONAL WAVES)
ONLY TRAVEL THROUGH SOLID
SURFACE WAVES
LOW FREQUENCY TRANSVERSE WAVES
SHADOW ZONE OF P WAVES
105 - 145
SHADOW ZONE OF S WAVES
105 - 105
AVERAGE DENSITY OF CRUST
2.7G/CM3
MOST ABUNDANT ELEMENTS ON EARTH’S CRUST
OS CIA
MOST ABUNDANT ELEMENTS ON EARTH
iOS
LITHOSPHERE
CRUST + UPPER PORTION OF MANTLE (10 - 200 km)
MANTLE
67% OF TOTAL MASS AND 83% OF TOTAL VOLUME
COMPOSED OF SILICATE ROCKS THAT ARE RICH IN Fe and Mg
DENSITY OF UPPER MANTLE
2.9 - 3.3 G/CM3
DENSITY OF LOWER MANTLE
3.3 - 5.7 G/CM3
ASTHENOSPHERE
EXTENDING UPTO 80 - 200KM
UPPER PORTION OF THE MANTLE
OUTER CORE
BETWEEN 2900 - 5100 KM
NIFE
LIQUID
DENSITY OF OUTER CORE
9.9 - 12.2G/CM3
EARTH’S MAGNETIC FIELD
CC IN OUTER CORE + CORIOLIS EFFECT
INNER CORE
PRMARILY IRON + NICAL
16% VOLUME & 33% OF THE MASS
DENSITY OF INNER CORE
12.6 - 13G/CM3
CRUST EXTENSION
0 - 70 KM
(OUTER CRUST : 0 - 35KM)
INNER CRUST: 35 - 70KM)
MANTLE EXTENSION
70 - 2900 KM
(OUTER MANTLE: 70 - 700KM)
(INNER MANTLE: 700 - 2900KM)
CORE EXTENSION
2900 - 6371 KM
(OUTER CORE: 2900- 5100KM)
(INNER CORE: 5100-6400 KM)
REPITI DISCONTIUITY
UPPER MATLE & LOWER MANTLE
GUTTENBERG DISCONTINUITY
LOWER MANTLE & OUTER CORE
CONORD DISCONTINUITY
UPPER CRUST & LOWER CRUST
MOHO DISCONTINUITY
LOWER CRUST & UPPER MANTLE
LEHMAN DISCONTINUITY
OUTER CORE & INNER CORE
AVERAGE DENSITY OF EARTH
5.51 G/CM3