Geologists have learned about Earth's interior structure using two main types of evidence: direct evidence from rock samples and indirect evidence from seismic waves. Rock samples provide clues about deep Earth conditions, as drills can reach over 12km deep and some rocks are blasted from over 100km deep. Seismic waves from earthquakes reveal the planet's structure based on their speed and paths through different layers. Geologists have determined Earth has three main layers - the crust, mantle, and core - which vary in size, composition, temperature, and pressure and surround each other like onion layers.

1. EARTH’S
INTERIOR

2. EXPLORING INSIDE EARTH
• Geologists have used two main types of
evidence to learn about Earth’s interior:
direct evidence from rock samples and
indirect evidence from seismic waves.

3. Evidence from Rock Samples…
• Rocks from inside Earth
give geologists clues about
Earth’s structure.
Geologists have drilled
holes as much as 12 km
deep into Earth. The drills
bring up samples of rock
that can be used to make
inferences about conditions
deep inside Earth.

4. • Sometimes, forces
inside Earth blast rocks
to the surface from
depths of more than
100 km. These rocks
provide more
information about
Earth’s interior.

5. Evidence from Seismic Waves…
• Since geologists cannot look inside Earth, they must
rely on indirect methods of observation. When
earthquakes occur, they produce seismic waves.
Geologists record seismic waves and study how they
travel through Earth. The speed of the seismic waves
and the paths they take reveal the structure of the
planet.

6. • Using data collected from seismic waves,
geologists have learned the Earth’s interior
is made up of several layers. Each layer
surrounds the layer beneath it, like the
layers of an onion.

7. A JOURNEY TO THE CENTER OF
THE EARTH
• The three main layers
of Earth are the crust,
the mantle, and the
core. These layers
vary greatly in size,
composition,
temperature, and
pressure.

8. Temperature…
• About 20 meters below Earth’s
surface, rock begins to get warmer.
For every 40 meters that you
descend from that point, the
temperature rises 1 degree Celsius.
This rapid rise of temperature
continues for several tens of km,
and continues to grow hotter and
hotter approaching the core. The
high temperatures inside Earth are
a result of heat left over from the
formation of the planet.

9. Pressure…
• The more you descend into Earth’s interior, the
amount of pressure increases. Pressure results
from a force pressing on an area. Because of
the weight of the rock above, pressure inside
Earth increases as you go deeper. The deeper
you go, the greater the pressure.

10. THE CRUST
• The crust is the layer
of rock that forms
Earth’s outer skin.
The crust is a layer of
solid rock that
includes both dry
land and the ocean
floor. This layer of
the Earth is much
thinner than the
layers beneath it.

11. • The crust beneath the ocean is called
oceanic crust, which consists mostly of
rocks such as basalt. Basalt is dark rock
with a fine texture.
BASALT

12. • Continental crust, crust that forms the
continents, consists mainly of rocks such as
granite. Granite is a rock that usually is light in
color and has a coarse texture.
GRANITE

13. THE MANTLE
• Below Earth’s crust is the mantle.
Earth’s mantle is made up of rock that
is very hot, but solid. Scientists divide
the mantle into layers based on the
physical characteristics of those
layers. Overall, the mantle is nearly
3000 km thick.

14. The Lithosphere…
• The upper most part of the mantle and the crust
together form a rigid layer called the
lithosphere. In Greek, “lithos” means “rock.”

15. The Asthenosphere…
• Below the lithosphere is a layer
that is hotter and under
increasing pressure. Like road
tar is softened by the heat of
the sun, this part of the mantle
is somewhat soft- it can bend
like plastic. This soft layer of
the mantle is called the
asthenosphere. In Greek,
“asthenes” means “weak.”
Although this layer is softer
than the rest of the mantle, it is
still solid.

16. The Lower Mantle…
• Below the asthenosphere, the
mantle is solid. This solid
material extends all the way to
Earth’s core.

17. THE CORE
• Beneath the mantle
is Earth’s core.
The core is made
mostly of the
metals iron and
nickel. It consist of
two parts- a liquid
outer core and solid
inner core.

18. The Inner and Outer Cores…
• The outer core is
a layer of molten
metal that
surrounds the
inner core.
Despite
pressure from
the rock above,
it is liquid.

19. • The inner core is a dense ball of solid metal. In
the inner core, extreme pressure squeezes the
atoms of iron and nickel so much that they
cannot spread out and become liquid.

20. The Core and Earth’s Magnetic
Field…
• Scientists believe
that movements in
the Earth’s liquid
outer core create
Earth’s magnetic
field. Because
Earth has a
magnetic field, the
planet acts as a
giant bar magnet.

21. VIDEO ANALYSIS
• https://www.youtube.com/watch?v=gMhou
zOiRjA
• https://www.youtube.com/watch?v=aY6SG
7GPAlo

23. • 1. Primary (P) Seismic Waves can pass through
____________________________.
• A) crust and core only
B) solids, gases, and liquids
C) liquids only
D) solids only
E) gases only
• 2. Secondary (S) Seismic Waves can pass through
____________________________.
• A) gases only
B) crust and core only
C) solids only
D) liquids only
E) solids, gases, and liquids

24. • 3. Of the 3 seismic waves, the _____-Waves are the
fastest.
• A) Q
B) L
C) P
D) R
E) S
• 4. P-Waves are also said to be ____________-
____________ waves.
• A) up-down
B) side-side
C) east-west
D) push-pull
E) north-south

25. • 5. The point within the earth where
seismic waves originate is called the
_____.
• A) origin
B) focus
C) fault scarp
D) epicenter