Rock Composition and Types How could you tell
- Slides: 21
Rock Composition and Types
How could you tell how many different types of rocks are in the photo? What characteristics would you look for?
What are Rocks? Rocks are: naturally formed non-living Earth material Rocks are made of collections of mineral grains and/or remains of living things held together in a firm solid mass.
How is a Rock Different from a Mineral? Rocks are made of minerals mineral grains can be microscopic to larger than your finger
Identifying Rocks are identified by: 1. Composistion: minerals they containeach type has some unique minerals 2. Texture: grain size is an important characteristic in all three types
Sample Materials Texture Formation Left Rock plagioclase, hornblende, pyroxene crystals visible to magma cooled naked eye slowly diorite Right Rock plagioclase, hornblende, pyroxene one type of crystal visible, rest microscopic andesite magma erupted and cooled quickly Rock Type
Three Types of Rocks Igneous Sedimentary Metamorphic
Igneous rocks All igneous rocks are the result of cooled magma or lava! Where the rock cools determines its appearance. Intrusive- cooled inside Earth’s crust Extrusive- cooled outside Earth’s crust
Igneous Rock Characteristics -spots or speckles -heavy or light -holes or solid -Colorful -smooth and glassy or rough and gritty
Why does it look like that composition of the minerals in the magma or lava how fast the magma or lava cools slower cooling = larger crystals faster cooling = smaller crystals
Igneous Rock Characteristics Intrusive= Slow cooling - Form inside crust - Coarse texture - Larger, visible crystals - Heavier - No holes - Light or dark colored depending on silica content Extrusive= Rapid cooling - Form outside crust - Fine texture - Small or no crystals - Very light - May have holes - Light or dark colored depending on silica content (high silica is lighter)
Sedimentary Rocks Formed by weathered sediments and dissolved minerals deposited into an area over time Compacted into layers over time Water can help cement sediments together
Sedimentary Rock Characteristics - Gritty, grainy, sandy texture - Made of sediment - Rough or smooth depending on size of sediment - Rock chuncks - Fossils - Layers - Not shiney - Earthy colors
Sedimentary Rock Formation • Clastic sedimentary rocks- composed of fragments and particles derived from preexisting rock- sandstone, conglomerate • Chemical sedimentary rocks- dissolved minerals carried to lakes and seas in rivers or ground water precipitates to form chemical sediments like salt or limestone • Organic sedimentary rock- made of living matter accumulated and compacted over timecoal, coquina
Transport & Deposition Sediments are transported by water, wind, ice or gravity Sediments will settle out of water when water slows. Sedimentary rocks form in layers with the youngest on the top
Sedimentary Rocks Reflect their Environment Beaches & deserts deposit sand Sediments from the bottoms of ponds, lakes, marshes, & swamps usually will be smaller and well sorted. Glaciers deposit sediment without sorting.
Metamorphic Rock Characteristics -sparkly -smooth -wavy or swirly layers -colorful -heavy -hard -solid -waxy
Metamorphic Rock Formation Heat and/or pressure change an existing rock into a metamorphic rock Change can be physical, chemical, or both Foliation can occur if the rock forms layers. Metamorphic rocks are either foliated or non-foliated.
Foliation
Metamorphic Diversity Metamorphic rocks are very diverse because there are some many different parent rocks that can be metamorphosed to various degrees.
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