Crust
Thinnest layerof the Earth
Made up of large amounts of silicon and aluminum
Composed of plates on which the continents and oceans rest.
These “ride” over molten mantle.
Crust is part of the lithosphere.
Two types of Crust: Oceanic and Continental
Ocean Land
Oceanic Crust Continental Crust
Oceanic Crust
Continental Crust
9.
Continental vs. OceanicCrust
Categor
y
Continental Oceanic
Rock Type Granite Basalt
Thickness 5 – 70km
(Thicker)
3 – 8 km
(Thinner)
State Solid Solid
Crust Age 4 billion years old
or Older
180 million years
old or Younger
Density Less Dense More Dense
Element Oxygen, Sodium, Iron,
10.
TheLithosphere
The crust andthe upper layer of the
mantle together make up a zone of
rigid, brittle rock called the
Lithosphere.
11.
The lithosphere (crustand upper
mantle) is divided into separate plates
which move very slowly in response to
the “convecting” part of the mantle.
12.
The Lithospheric Plates
Thecrust of the Earth is broken into many pieces called plates. The
plates "float" on the soft, semi-rigid asthenosphere.
The Mantle
The Mantleis the
largest layer of the Earth
at 2900 km thick. The
middle mantle is
composed of very hot
dense rock that flows like
asphalt under a heavy
weight. The movement of
the middle mantle
(asthenosphere) is the
reason that the crustal
plates of the Earth move.
Asthenosphere
The asthenosphere (“weaksphere”) is a soft layer of the
mantle on which pieces of the lithosphere move. It is made
of solid rock that, like putty, flows slowly- at about the same
rate your fingernails grow.
17.
Convection Currents
The middlemantle "flows" because of convection
currents. Convection currents are caused by the very
hot material at the deepest part of the mantle rising being
less dense, then cooling becoming more dense and
sinking again --repeating this cycle over and over.
18.
Mantl
e
Solid butcapable of flow (like fudge) Semi-Solid/Semi Liquid
Thickest layer of the Earth 2900km (1800 miles)
Element Composition: Magnesium, Silicon, Oxygen, and Iron
The hot magma rises then cools and sinks.
These convection currents cause changes in the Earth’s
surface.
Conveyor belt for the tectonic plates.
Upper Mantle
Convection
Currents
Middle
Mantle
Lower Mantle
Outer
Core
Composition: Molten (liquid)metal
that is about 4,700°C (8,500°F)
Thickness: 2,266 km (1,400) miles
State of Matter: Composed of the
melted metals nickel and iron (liquid)
Located about 1,800 miles beneath
21.
Inner
Core
Solid spheremade mostly of iron and has
Nickel
It is believed to be as hot as 6,650°C
(12,000°F)
Heat in the core generated by the
radioactive decay of uranium and other
elements
23.
What do thesetwo images tell
us about the layers of the Earth?
Add this statementto the
arrow going down on your
foldable.
Temperature,
Density and
Pressure increases
as depth increases
27.
Which layer ofthe Earth has the
greatest temperature, pressure, and
density?
Core
28.
How do weknow so much about
what’s under Earth’s surface?
• Through INDIRECT EVIDENCE, mostly
from seismic waves caused by earthquakes
(more on this later this semester...)
• Sometimes indirect evidence is the only
option for scientists to develop a theory
• Lets give it a try...
29.
Big Ideas
• TheEarth is divided into 3 Main Layers
– Crust
– Mantle
– Core
• Main Rock type of the 2 types of Crust
– Oceanic – Basalt
– Continental – Granite
• Oceanic Crust is denser than Continental Crust
30.
Big Ideas Continued
•The lithosphere is divided into tectonic plates.
• The Mantle has the convection currents which causes the plates to
move.
• The Asthenosphere flows semi-liquid on which the plates move
• Temperature, pressure, and density increases as depth increases. This is
a direct relationship.
Editor's Notes
#10 In depth teaching about the plates and their movement will occur in the next essential question
#20 The movement of the lithospheric plates and the convection currents will be covered more in-depth during the next essential question.