Tectonic Hazards
Weather Hazards
Pattern of fossils
Who am I
re- order
100

massive wave that can cause damage when it reaches the land 

Tsunami 

100

are funnel-shaped wind storms that reach from clouds to the ground.

Tornadoes 

100

Most fossils are found within

Sedimentary rocks 

100

a long period of very dry weather.

Drought 

100

…..   A fossil forms .

…… Soft tissue decays .

……. Bones are replaced by minerals 

……… An organism dies.

4

2

3

1

200

causes the crust to shake.

An earthquake 

200

the sudden sliding of snow, ice, and rock down a slope.

Avalanche 

200

……… from deep underground can cool and harden into igneous rocks

Magma 

200

The top part of large pieces of rock called tectonic plates.

Crust

200

Large ocean waves slow down and increase in height as they reach coast.

Two tectonic plates slide past each other underwater.

1

300

an opening in earth’s crust that allows superheated materials to reach the

surface

Volcano 

300

 a snowstorm with high winds. 

Blizzard 

300

are impressions such as footprints, burrows, or nest

Trace Fossils 

300

 Can change sedimentary rocks into

metamorphic rocks.

Heat and Pressure 

300

Which layer is the oldest ?

Layer C

Layer B

Layer A

Layer A

400

An earthquake's energy is measured on

Magnitude Scale 

400

Hurricanes can cause a rise in the local sea level is called

Storm surge 

400

In sedimentary strata the layers of rocks are in …………………. pattern 

Horizontal 

400

The sandbags placed in front of the house will most likely prevent………

Flooding 

400

Metamorphic rocks 

Sedimentary 

2

500

- Which rating of earthquake that cause the bookcase fell and some dishes were broken in the kitchen?

M 3 

M 5.1 

M 7.5

M 9

500

caused by heavy rain bombarding loose soil

Landslide

500

How do scientists determine the age of fossils and rock layers?

By examining the order of layers 

500

The earthquake most likely started at ……….

Fault 

500

Stress causes along the fault 

Stress is released causes crust to shake

Continuous movement of tectonic plates

2

3

1

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