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Notes 5-2 VocabularyTerms

Misc.

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Notes 5-3Notes 5-1

Deformation

The crust is the bending, tilting,

and braking of the earth’s crust.

Plate

movement

What causes stress on

the earth’s surface

crust.

Stress

What cause strain

on the crust.

Compression

What occurs when

crustal rocks are

Squeezed together?

Tension

What is the force

that pulls the rocks

apart.

Deformed

In extreme stress, rock

becomes so What? it

may break.

Folding

When rocks respond to

stress by becoming

permanently deformed

without breaking it is

called what?

Rock

In extreme stress, What

becomes so deformed it

may break.

Stress

When What is applied

slowly, the deformed rock

will return to it’s original

shape.

What is a down curved fold in which the youngest layer is in the center

Syncline

What is a down curved fold in which the youngest layer is in the center.

Mountain Range

A group of adjacent

mountains with the

same general

Continents

Mountains can

also form when

two what

collide?

Mountain

System

a group of

adjacent

mountain

ranges.

Mountain Belts

the largest mountain

system are part of

two still larger

systems.

Molten Rock

Mountains that form

when What erupts

onto the earth

surface.

Anticline

Upcurve fold in which the

oldest layer is in the center of the of the fold

Syncline

A down curved fold in which the youngest layer is in the

center

Monocline

A fold in which both limbs

remain horizontal or

vertical.

Normal Fault

Hanging wall moves down

relative to the footwall along

divergent boundaries

Reverse Fault

Compression causes the

hanging wall to move up relative

to the footwall

Footwall

rock below the

fault plane of a

nonvertical fault

Thrust Fault

Fault plane is a low angle or nearly

horizontal & hanging wall is pushed up over

rock

Strike-slip fault

rock on either side of the fault plane

slides horizontally at transform boundaries

Hanging wall

rock above the

fault plane of a

nonvertical

fault

Fault

when rocks do

not move

Make your wager

Fracture

No movement in

the rocks along

either side of a

break.