Internal Structure of Earth

Deep parts of Earth are studied indirectly, however, largely through the branch of geology called geophysics

1. Internal structure of earth A Schematic view of interior of earth CRUST MANTLE OUTER CORE INNER CORE

2.  Deep parts of Earth are studied indirectly, however, largely through the branch of geology called geophysics.  Geophysics includes the study of seismic waves and Earth’s magnetic field, gravity, and heat.  Together, they create a convincing picture of what makes up Earth’s interior. Introduction  There are two important ways of learning about Earth’s interior. 1.seismic reflection 2.Seismic refraction

3. By seismic study earth has following layers: 1-The crust Continental crust Oceanic crust 2-The mantle Upper mantle Lower mantle 3-The core Outer core Inner core

4.  Studies of seismic waves have shown that the crust is thinner beneath the oceans as compare to the continents. The Crust  The uppermost layer of earth is called crust.  Seismic waves travel faster in oceanic crust than in continental crust. On this basis crust is divided into two types. Continental crust Oceanic crust  Seismic P waves travel through oceanic crust at about 7km/s & about 6km/s through continental crust.

5.  Lithosphere  The combination of uppermost mantle and crust above the asthenosphere is called the lithosphere .  The lithosphere is free to move over the weak asthenosphere.  The tectonic plates are, in. fact, lithospheric plate  The boundary that separates the crust from the mantle is called the Mohorovic˘ic ´ discontinuity.  Moho Boundary:

6. Properties of the Crust:  Continental Crust: ► Depth 20 to 70 km, average 30 to 40 km ► Composition: felsic, intermediate, and mafic igneous, sedimentary, and metamorphic rocks. ► Age: 0 to 4 B.y. ► Summary: thicker, less dense, heterogeneous,  Oceanic Crust: ► Depth to Moho: ~7 km ► Composition: mafic igneous rock (basalt & gabbro) with thin layer of sediments on top ► Age: 0 to 200 M.y . ► Summary: thin, more dense, homogeneous,

7. The Mantle:  The next layer below the crust is mantle.  Its thickness extended to a depth of 2890km.  It is more denser than crust  It consist of dense silicate rocks both p-waves & s-waves travel through the mantle  depths of around 100 km to 250 km arrive later than expected (because pressure is increasing) indicating a zone of low seismic wave velocity.

8. Velocity of seismic waves in mantle:  P -waves velocity: Its velocity is about 8km/s in the upper mantle and increases up to 13km/s in lower mantle  S -waves velocity: S-waves velocity profile in the mantle is similar to the p-wave profile. S-waves velocity time cannot be measured as accurately as p-waves travel time.

9. The core The central or innermost portion of earth below the mantle is core it lies at depth of 2900km up to 6370km the core is divided into two layers outer core inner core Outer core:  The outer core begins at a depth of 2,890 to 5,150 km.  The temperature at outer core is about 3700˚C Inner core:  The inner section begins at a depth of 5,150 to 6,360km.  The temperature of inner core is about 4300˚C.

10.  Seismologists first determined that the back and-forth motion of S-waves does not travel through liquid.  Then, seismologists noticed that S-waves do not travel through Earth’s center.  This observation led to the discovery that Earth’s core must be at least partly liquid. Evidence of Liquid Outer core: