The Rock Cycle Dustin Palik 6 th Grade Science
E.SE Compare and contrast the formation of rock types (igneous, metamorphic, and sedimentary) and demonstrate the similarities and differences using the rock cycle model. SWBAT list the three main rock types. SWBAT compare and contrast the formation of the three main rock types. SWBAT demonstrate the similarities and difference using the rock cycle model. Click here to start presentation
The Rock Cycle Click each heading for more information Heat and Pressure Weathering and Erosion Igneous Sedimentary Metamorphic Go to end
The Rock Cycle Click each heading for more information Heat and Pressure Weathering and Erosion Igneous Sedimentary Metamorphic Go to end
The Rock Cycle Click each heading for more information Heat and Pressure Weathering and Erosion Igneous Sedimentary Metamorphic Go to end
The Rock Cycle Click each heading for more information Heat and Pressure Weathering and Erosion Igneous Sedimentary Metamorphic Go to end
The Rock Cycle Click each heading for more information Heat and Pressure Weathering and Erosion Igneous Sedimentary Metamorphic Go to end
The Rock Cycle Click each heading for more information Heat and Pressure Weathering and Erosion Igneous Sedimentary Metamorphic Go to end
The Rock Cycle Click each heading for more information Heat and Pressure Weathering and Erosion Igneous Sedimentary Metamorphic Go to end
The Rock Cycle Click each heading for more information Heat and Pressure Weathering and Erosion Igneous Sedimentary Metamorphic Go to end
The Rock Cycle Click each heading for more information Heat and Pressure Weathering and Erosion Igneous Sedimentary Metamorphic Go to end
The Rock Cycle Click each heading for more information Heat and Pressure Weathering and Erosion Igneous Sedimentary Metamorphic Go to end
Igneous Rock Commonly called “fire rocks” Formed underground by cooling of magma Formed above ground by cooling of lava Examples: GranitePumice ScoriaObsidian Return to main
Metamorphic Rock Rocks have morphed from another type Formed after extreme heat and pressure Examples: SchistGneiss Return to main
Sedimentary Rock Weathering and erosion turn rocks into sediment Sediments settle into layers over time Formed after long periods of time in lowest levels Examples: SandstoneLimestone ShaleConglomerate Return to main
Melting and Cooling Magma Return to main
Melting and Cooling Magma Return to main
Melting and Cooling Magma Return to main
Melting and Cooling Magma Return to main
Melting and Cooling Magma Igneous rock forms as magma/lava cools Return to main
Heat and Pressure Igneous rock Return to main
Heat and Pressure Igneous rock Return to main
Heat and Pressure Igneous rock Return to main
Heat and Pressure Igneous rock morphing under pressure Return to main
Heat and Pressure Metamorphic rock Return to main
Weathering and Erosion Metamorphic or Igneous Rock Return to main
Weathering and Erosion Rain Wind Continuous weathering begins to break down the rock into sediments Return to main
Weathering and Erosion Sediment can be carried away by wind or water and deposited Return to main
Weathering and Erosion As more and more rock is weathered and eroded, deposits begin to form layers Return to main
Weathering and Erosion More layers result in increased depth and pressure Return to main
Weathering and Erosion The bottom most layer eventually cements together to form a new type of rock – Sedimentary Rock Return to main
Bibliography Payton, T. (1998, August 8). Rock hounds. Retrieved from Hit ESC key to exit