1.COMPOSITION-PERCENTAGE OF WHAT MINERALS ARE INSIDE.. **DRAW THE COMPOSITION OF EACH OF YOUR SAMPLES. 2.TEXTURE-SIZE AND SHAPE OF THE GRAINS INSIDE ROCK DRAW FINE-GRAINED, MEDIUM-GRAINED AND COARSE-GRAINED SAMPLES... 2.FINE-GRAINED TEXTURECAN'T SEE WHAT IS INSIDE MEDIUM-GRAINED TEXTURECAN SEE SOME, BUT NOT ALL COARSE-GRAINED TEXTURECAN EASILY SEE ALL INSIDE 3. IGNEOUS ROCK=FORMED BY COOLING... EXTRUSIVE-COOLS FAST, LAVA ERUPTED(OUTSIDE OR ON SURFACE), TINY CRYSTALS, FINE-GRAINED TEXTURE... DRAW THIS TYPE OF IGNEOUS ROCK 4.IGNEOUS ROCK=FORMED BY COOLING... INTRUSIVE IGNEOUS=SLOW COOLING, MAGMA(INSIDE EARTH), LARGE CRYSTALS, COARSE GRAINED TEXTURE...DRAW A SAMPLE OF THIS... 5.IGNEOUS ROCK=FORM BY COOLING(ABOVE OR BELOW SURFACE) FELSIC IGNEOUS=LIGHT IN COLOR, LESS DENSE MAFIC IGNEOUS= DARK IN COLOR, MORE DENSE.. DRAW EACH... 7.SEDIMENTARY ROCKS=FORMED BY.. W=WEATHERING E=EROSION D=DEPOSITION C=COMPACTION C=CEMENTATION DRAW WEATHERING= BREAKING DOWN OF BIG ROCK INTO SMALL PIECES(SEDIMENTS) 8.SEDIMENTARY ROCKS=FORMED BY.. W=WEATHERING E=EROSION D=DEPOSITION C=COMPACTION C=CEMENTATION DRAW WEATHERING= BREAKING DOWN OF BIG ROCK INTO SMALL PIECES(SEDIMENTS) 9.SEDIMENTARY ROCKS=FORMED BY.. W=WEATHERING E=EROSION D=DEPOSITION C=COMPACTION C=CEMENTATION DRAW EROSION-MOVEMENT OF SEDIMENT(SMALL ROCK) TO ANOTHER PLACE BY WIND, WATER, GRAVITY, ICE 10.SEDIMENTARY ROCKS=FORMED BY.. W=WEATHERING E=EROSION D=DEPOSITION C=COMPACTION C=CEMENTATION DRAW DEPOSITION=WHEN SEDIMENT(SMALL ROCK) DROPS AND DEPOSITS, SETTLES AT BOTTOM OF ANOTHER BODY OF WATER(USUALLY FALLS IN LAYERS) 11.SEDIMENTARY ROCKS=FORMED BY.. W=WEATHERING E=EROSION D=DEPOSITION C=COMPACTION C=CEMENTATION DRAW COMPACTION= ROCK PIECES(SEDIMENTS) PRESSED OR SQUEEZED TOGETHER 12.SEDIMENTARY ROCKS=FORMED BY.. W=WEATHERING E=EROSION D=DEPOSITION C=COMPACTION C=CEMENTATION DRAW CEMENTATION= WHEN ROCK PIECES(SEDIMENTS) ARE LIKE GLUED OR STICK TOGETHER 13.STRATIFICATION IN SEDIMENTARY ROCKS- WHEN SEDIMENTARY ROCKS HAVE “LAYERING” CALLED STRATA... DRAW THE STRATIFICATION YOU SEE IN YOUR ROCK SAMPLE... 14.SUPERPOSITION IN SEDIMENTARY ROCKS= WHEN YOUNGER ROCKS LAY ON TOP AND OLDER ROCKS GET COMPACTED OR SQUEEZED TO THE BOTTOM... EXAMPLE= YOUNGEST ON TOP OLDER EVEN OLDER OLDEST LAYER ON BOTTOM DRAW SUPERPOSITION IN YOUR ROCK SAMPLE... 15.TYPES OF SEDIMENTARY ROCKS... CLASTIC- FORM WHEN ROCK FRAGMENTS ARE SQUEEZED TOGETHER... DRAW THIS SAMPLE OF CLASTIC YOU SEE HERE... 16.TYPES OF SEDIMENTARY ROCKS... CHEMICAL=FORMED WHEN DISSOLVED MINERALS CRYSTALLIZE... DRAW YOUR SAMPLE OF CHEMICAL YOU SEE HERE... 17.TYPES OF SEDIMENTARY ROCKS... ORGANIC=FORMED FROM THE REMAINS OF LIVING THINGS(FOSSILS) DRAW YOUR ORGANIC(FOSSIL) SEDIMENTARY ROCK YOU SEE HERE... 18.SEDIMENTARY ROCKS OFTEN APPEAR “EARTHY” IN APPEARANCE, CAN HAVE LAYERING AND FOSSILS...DRAW ANY OF THESE FEATURES YOU SEE HERE... 20.METAMORPHIC ROCK=CHANGED SHAPE FROM ONE ROCK TO ANOTHER... BY HEAT AND PRESSURE... METAMORPHIC ROCKS ARE OFTEN FLAT AND HARD... DRAW WHAT YOU SEE HERE... 21.METAMORPHIC ROCK=CHANGED SHAPE FROM ONE ROCK TO ANOTHER... BY HEAT AND PRESSURE... FOLIATED METAMORPHIC= GRAINS ARE IN BANDS/LINES DRAW THIS SAMPLE THAT YOU SEE HERE 22.METAMORPHIC ROCK=CHANGED SHAPE FROM ONE ROCK TO ANOTHER... BY HEAT AND PRESSURE... NON-FOLIATED METAMORPHIC= FLAT WITH NO LINES OR BANDS DRAW AN EXAMPLE OF THIS... METAMORPHIC ROCKS OFTEN FORM DEEP DOWN INSIDE THE EARTH WHERE THE TEMPS AND PRESSURE ARE VERY HIGH... DRAW YOUR BEST IMAGE OF THIS... IGNEOUS=FORM BY COOLING OF MAGMA OR LAVA DRAW LAVA=EXTRUSIVE IGNEOUS=COOLS FAST, SMALL CRYSTALS, FINE-GRAINED TEXTURE, OUSIDE SURFACE DRAW MAGMA=COOLS SLOW, BIG CRYSTALS, INSIDE EARTH, COARSE-GRAINED, INTRUSIVE IGNEOUS SEDIMENTARY ROCKS FORM ON OR ALONG EARTH'S SURFACE AND CAN HAVE FOSSILS AND BE FOUND IN LAYER UPON LAYER UPON LAYER... YOUNGEST LAYER ON TOP OLDER LAYER EVEN OLDER OLDEST LAYER ON BOTTOM…DRAW YOUR BEST IMAGE OF THIS