GEOLOGY MACC Bill Palmer

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GEOLOGY MACC Bill Palmer Lecture 4 Rocks

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GEOLOGY MACC Bill Palmer. Lecture 4 Rocks. What are Rocks?. Rocks are solid materials that comprise nearly all of the earth (and moon and planets). Rocks are almost always aggregates of minerals. (This is why we study minerals first). What is the Rock Cycle?. - PowerPoint PPT Presentation

Transcript of GEOLOGY MACC Bill Palmer

GEOLOGYMACC

Bill Palmer

Lecture 4Rocks

What are Rocks?Rocks are solid materials that comprise nearly all of

the earth (and moon and planets).

Rocks are almost always aggregates of minerals.(This is why we study minerals first).

What is the Rock Cycle? The rock cycle explains how all rocks can be

formed, deformed transformed, destroyed, and reformed as a result of natural processes.

Rock CycleMaterials for forming rocks comes from:

1) the Earth’s mantle (molten rock is magma when in the ground and lava when it erupts on the surface)

2) Space (meteorites)3) Organisms (plants and animals) 4) Fragmentation and decay of other rocks and minerals

Rock CycleThere are three main rock groups:

1) IGNEOUS ROCKS –Form when magma or lava cool.

2) SEDIMENTARY ROCKS- Form when chemical residues and fragments of plants, animals, crystals, or rocks, or sand are compressed and cemented together. Also form from chemical precipitation.

3) METAMORPHIC ROCKS- Form when other rocks are changed by heat, pressure, or hot fluids.

The Rock Cycle

Rock Properties 1. General form-smooth, rough, irregular 2. Color-light, dark, 3. Grains-sand, gravel, crystals, fossils, fragments 4. Shape-teardrop, icicle, smooth, sphere

Rock Properties 5. Texture is very important-

GlassyFine-grained , <1mmCoarse-grained, >1mmVesicular-bubblesFoliated-layersClastic-”clasts” of plants, animals, minerals

Igneous Rocks Intrusive Igneous Rocks-Magma is the source

and the rocks cool slowly beneath the ground and form large crystals.

Extrusive Igneous Rocks-Lava is the source and the rocks cool quickly above the ground and form small crystals.

INTRUSIVE STRUCTURES1. Batholith-Massive, no “bottom” 2. Sills-Sheet-like between layers of other rocks3. Laccolith- “Blister-like”4. Pipe-vertical tube5. Dikes-Layers vertical to rock

1. Radial2. Sheet3. Ring

EXTRUSIVE Lava Flows Pyroclastic deposits (fire fragments)

How to Analyze Igneous Rocks STEP 1 and 2-Study the Color and Mineral

CompositionLight- Felsic Minerals (feldspar)

Quartz (gray, white)Plagioclase Feldspar (white)Potassium Feldspar (pink)Muscovite Mica (clear, brownish)

How to Analyze Igneous Rocks STEP 1 and 2-Study the Color and Mineral

CompositionDark-Mafic Minerals (no feldspar)

Biotite Mica (black)Amphibole (dark gray)Pyroxene (dark green)Olivine (green)

How to Analyze Igneous Rocks STEP 3-Study the Texture

IntrusivePegmatitic (crystals >1 cm)Phaneritic (crystals 1-10 mm)Porphyritic (large and small crystals indicate that it cooled at

TWO different rates)

How to Analyze Igneous Rocks STEP 3-Study the Texture

ExtrusivePorphyritic (large and small crystals indicate that it cooled at

TWO different rates)Aphanitic (crystals < 1mm)Glassy (like glass, crystals too small to see)Vesicular (small or large bubbles, like pie meringue or froth)Pyroclastic- particles emitted from volcano

Now, put it all together!

Now, put it all together!

Some Igneous Rocks to Know Granite Gabbro Rhyolite Basalt Scoria Pumice Rhyolite Porphyry

Wrap-ups1. What are rocks?2. What is the Rock Cycle?3. What is the difference between magma and lava?4. What are the three types of rocks?5. What is a batholith? Sill? Laccolith?

Wrap-upsName the rock described:

6. Light colored, coarse grained.7. Dark colored, coarse grained.8. Light colored, very fine grained9. Spongy looking and light in color.10. Dark and glassy looking.