Story in the Rocks By: Riley Fanning, Maria Ezzell, Robbie Himebaugh.

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Story in the Rocks By: Riley Fanning, Maria Ezzell, Robbie Himebaugh

Transcript of Story in the Rocks By: Riley Fanning, Maria Ezzell, Robbie Himebaugh.

Page 1: Story in the Rocks By: Riley Fanning, Maria Ezzell, Robbie Himebaugh.

Story in the RocksBy: Riley Fanning, Maria Ezzell, Robbie Himebaugh

Page 2: Story in the Rocks By: Riley Fanning, Maria Ezzell, Robbie Himebaugh.

Rock Cycle/TypesThe Rock Cycle is the formation,

breakdown, and reformation of rocks.

The 3 types of rocks include Igneous, Sedimentary, and Metamorphic.

Page 3: Story in the Rocks By: Riley Fanning, Maria Ezzell, Robbie Himebaugh.

Igneous Rocks

A rock that forms after magma/lava cools.

Page 4: Story in the Rocks By: Riley Fanning, Maria Ezzell, Robbie Himebaugh.

Metamorphic Rocks

A rock that forms under a lot of pressure and heat.

Page 5: Story in the Rocks By: Riley Fanning, Maria Ezzell, Robbie Himebaugh.

Sedimentary Rocks

A rock that forms from compacted pieces of sediment.

Page 6: Story in the Rocks By: Riley Fanning, Maria Ezzell, Robbie Himebaugh.

WeatheringWeathering is two process

(chemical and physical) that often work in concert to decompose rocks.

Chemical Weathering – involves a chemical change in at least some of the minerals within a rock.

Physical Weathering – physically breaking rocks into fragments.

Page 7: Story in the Rocks By: Riley Fanning, Maria Ezzell, Robbie Himebaugh.

ErosionErosion is simple movement to a

slope due to gravity. (Mass Wasting)

Sheet Erosion – a type of soil erosion on sloping farmland, in which rain washes the top layer of soil off.

Sheet Erosion

Page 8: Story in the Rocks By: Riley Fanning, Maria Ezzell, Robbie Himebaugh.

Geologic Time ScaleThe Geologic Time Scale is a

chart that shows the eons, eras, epochs, and pivotal events, that happened in that time period.

Page 9: Story in the Rocks By: Riley Fanning, Maria Ezzell, Robbie Himebaugh.

FossilsA Fossil is an imprint that shows

bones, shells, animals etc. on rocks.

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SuperpositionThe Law of Superposition is

the bottom layer of rocks are older than the top layer of rocks.

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http://questgarden.com/66/40/8/100215071121/process.htm http://www.nature.nps.gov/geology/usgsnps/misc/gweaero.html http://www.answers.com/topic/sediment http://www.watersheds.org/earth/erosion.htm http://www.answers.com/topic/sheet-erosion http://en.wikipedia.org/wiki/Erosion http://scienceguy288.wordpress.com/2008/01/29/north-america-

trip-1-the-grand-canyon/ http://imnh.isu.edu/digitalatlas/geo/basics/diagrams.htm http://www.gsa.org.au/resources/factites/factitesRocks.pdf http://www.fi.edu/fellows/fellow1/rocks/create/igneous.htm http://www.fi.edu/fellows/fellow1/oct98/create/metamorph.htm http://answers.yahoo.com/question/index?qid=20071216203637

AAUvTKD http://www.enchantedlearning.com/subjects/Geologictime.html www.google.com/images