rocking with rocks!

21
ROCKING WITH ROCKS! Table of Contents #7

Upload: ormand

Post on 24-Feb-2016

70 views

Category:

Documents


0 download

DESCRIPTION

Table of Contents #7. Rocking with rocks!. What are igneous, sedimentary, and metamorphic rocks and which picture is a representation of that rock type. C. A. B. Igneous - think of the word “ignites” Formed from solidified molten rocks Metamorphic – Think of the word “magma” - PowerPoint PPT Presentation

TRANSCRIPT

Page 1: Rocking with rocks!

ROCKING WITH ROCKS!

Table of Contents #7

Page 2: Rocking with rocks!

What are igneous, sedimentary, and metamorphic rocks and which picture is a representation of that rock type.

A

B

C

Page 3: Rocking with rocks!

TYPES OF ROCK Igneous -

think of the word “ignites” Formed from solidified molten rocks

Metamorphic – Think of the word “magma” Formed when other rocks are changed by heat, pressure, and

chemical reactions within the Earth

Sedimentary - Formed when combinations of rock fragments, seashells, and

chemicals are composed in layers and hardens

Page 4: Rocking with rocks!

SOMETHING TO THINK ABOUT… Out of the three types of rocks, which

one do you think will have fossils? Explain which rock type you chose and why the others wouldn’t have any.

Page 5: Rocking with rocks!

THE EARTH’S STORY

Uniformitarianism

Theory: Geologic change is gradual

Scientist: Hutton

To help me remember:

think of uniform

Catasrophism

Theory: Geologic change is sudden

Scientist: Lyell

To help me remember:

Think of catastrophe (disaster)

Page 6: Rocking with rocks!

CURRENT THEORY Modern geology (current theory):

Gradual geologic change is interrupted by catastrophes

To study geologic change involves studying past life. Using fossils to study past life is called paleontology.

Page 7: Rocking with rocks!

RELATIVE DATING Relative Dating: what scientist use to

determine whether an event or object is older or younger than another event or object

Relative Dating is just an ESTIMATE of events… There is no absolute information

Page 8: Rocking with rocks!

LAW OF SUPERPOSITION The Law of Superposition states:

Younger rock lies above older rock in an undisturbed sequence.

Page 9: Rocking with rocks!
Page 10: Rocking with rocks!

GEOLOGIC COLUMN Geologic column is an arrangement of

rock layers in which the older rocks are at the bottom

Geologic columns help scientist find the relative age of the Earth.

Page 11: Rocking with rocks!

SO WHAT ABOUT DISTURBED ROCK? Features:

Faults – break in the Earth’s crust, where blocks of crust shift past one another

Page 12: Rocking with rocks!

FEATURES Intrusion – Igneous rock (molted rock)

from the Earth’s interior that squeezes into existing rock and cools (younger then sedimentary layers)

Page 13: Rocking with rocks!

EVENTS Folding – Occurs when rock layers bend

and buckle from Earth’s internal forces

Page 14: Rocking with rocks!

EVENTS Tilting -occurs when Earth’s forces

move rock layers until they become slanted.

Page 15: Rocking with rocks!

CROSS CUTTING LAW Any feature that cuts across a body of

sediment or rock is younger than the body of sediment or rock that it cuts

Page 16: Rocking with rocks!

LIST THE LAYERS FROM YOUNGEST TO OLDEST

A

B

C

D

E

F

G

Page 17: Rocking with rocks!

LIST THE LAYERS FROM YOUNGEST TO OLDEST

Page 18: Rocking with rocks!

RECAP: IS THE ROCK IN THIS PICTURE DISTURBED? IF SO, EXPLAIN HOW.

Page 19: Rocking with rocks!

HOW ABOUT NOW?

Page 20: Rocking with rocks!

LAST ONE…

Page 21: Rocking with rocks!