rocking the internet sherry wisdom etec 557 fall 2010 tamu-c

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Rocking the Internet Sherry Wisdom ETEC 557 Fall 2010 TAMU-C

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Page 1: Rocking the Internet Sherry Wisdom ETEC 557 Fall 2010 TAMU-C

Rocking the Internet

Sherry WisdomETEC 557

Fall 2010 TAMU-C

Page 2: Rocking the Internet Sherry Wisdom ETEC 557 Fall 2010 TAMU-C

Goals & Objectives

• Goal(s) The student will be able to classify rocks as metamorphic, igneous, or sedimentary by the processes of their formation. The student will also communicate using various forms of effective technology related communication.

• Objective(s) Students in collaborate learning groups will collect information about the rock cycle and complete the provided Word template. The student uses technology to produce a PowerPoint presentation based on the Word template, and assessed through a provided rubric.

Page 3: Rocking the Internet Sherry Wisdom ETEC 557 Fall 2010 TAMU-C

The Rock Cycle

Page 4: Rocking the Internet Sherry Wisdom ETEC 557 Fall 2010 TAMU-C

Types of RocksRocks are not all the same!

SedimentarySedimentary rocks are formed from particles of sand, shells, pebbles, and other fragments of material. Together, all these particles are called sediment. Gradually, the sediment accumulates in layers and over a long period of time hardens into rock. Generally, sedimentary rock is fairly soft and may break apart or crumble easily. You can often see sand, pebbles, or stones in the rock, and it is usually the only type that contains fossils. Examples of this rock type include conglomerate and limestone.

MetamorphicMetamorphic rocks are formed under the surface of the earth from the metamorphosis (change) that occurs due to intense heat and pressure (squeezing). The rocks that result from these processes often have ribbon like layers and may have shiny crystals, formed by minerals growing slowly over time, on their surface. Examples of this rock type include gneiss and marble.

IgneousIgneous rocks are formed when magma (molten rock deep within the earth) cools and hardens. Sometimes the magma cools inside the earth, and other times it erupts onto the surface from volcanoes (in this case, it is called lava). When lava cools very quickly, no crystals form and the rock looks shiny and glasslike. Sometimes gas bubbles are trapped in the rock during the cooling process, leaving tiny holes and spaces in the rock. Examples of this rock type include basalt and obsidian.

Page 6: Rocking the Internet Sherry Wisdom ETEC 557 Fall 2010 TAMU-C

Let‘s Put it Together

• http://www.learner.org/interactives/rockcycle/diagram.html

This is an interactive site we can visit together and by rolling the mouse over the picture, we can

make the rock cycle work and see how rocks are formed.

Page 7: Rocking the Internet Sherry Wisdom ETEC 557 Fall 2010 TAMU-C

Ricky the Rapping Rock

Let’s visit Ricky and see how he raps the rock cycle. Then let’s see if we

can come up with our own rap.

http://www.msnucleus.org/membership/storybooks/ricky.html