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The Rock Cycle

TermDefinition
sedimentary rock ​rocks made from layers of sand, mud, shells, or tiny pieces of other rocks that get pressed together
metamorphic rock rocks that were once another type of rock but changed because of strong heat and pressure
igneous rock rocks that form from melted lava or magma that cools and harden
weathering when rocks are broken down into smaller pieces by wind, water, ice, or other living things
erosion when wind, water, or ice move broken rock and soil from one place to another
compaction when bits of sand, mud, or other sediments get pressed tightly together by weight on top of them
cementation when water mixes together with particles and crystalize, filling gaps and acting like glue forming new rocks and holds them together
The Rock Cycle the way rocks change from one kind to another over a long time; Rocks can melt, get squished, break apart, or cool down, and that’s how they become new types of rocks
deposition when rocks, sand, or soil are dropped in a new place by wind, water, or ice
lava hot, melted rock that has come out of a volcano and onto the surface
magma hot, melted rock that is under the ground
Law of Superposition In layers of rocks, the bottom layers are the oldest and the top layers are the youngest.
Law of Crosscutting If a rock layer or fault cuts across other layers, it is younger than the layers it cuts through.
Law of Inclusions If a rock has pieces of another rock inside it, the pieces are older than the rock that surrounds them.
Relative Dating Relative dating tells us which rock or fossil is older or younger compared to others, but not the exact age.
Absolute Dating Absolute dating tells us the exact age of a rock or fossil in years.
Volcanic Dyke A volcanic dike is a wall of magma that pushed up through cracks in rocks and then hardened.
Created by: user-1981613
 

 



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