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Chapter 19
Section 3
Identify the three types of rocksExplain the properties of each type of rock
based on physical and chemical conditions under which the rocks were formed
Describe the rock cycle and how rocks change form
Explain how the relative and absolute ages of rocks are determined
MineralIgneous rockWeatheringSedimentary rockFossilsMetamorphic rock
Rocks are composed of mineralsThey are naturally occurring, non-living
substances that have a chemical formulaThere are about 3500 minerals in the Earth’s
crustOnly about 20 are easily found in a pure stateSome rocks are composed of more than 1 mineral
Minerals form crystalsThe top nine are found quite easily
Feldspar, pyroxene, mica, dolomite, quartz, amphibole, clay, and calcite
CharacteristicsRocks may be porous, granular, or smoothThey may be soft or hardThey may have different densities or colors
There are three major types of rockIgneous, formed from molten or melted rockSedimentary, formed from the remains of other
rocks or organismsMetamorphic, formed from pressure and
heating
Obsidian Igneous Rock Black, extrusive
igneous rock Obsidian is often
called volcanic glass due to its absent crystals and glassy appearance
Major minerals include feldspar, quartz and mica
Sandstone Sedimentary Rock
Red, banded sample is due to iron oxidation
Sandstone is formed from beach sand-sized quartz grains that are glued together with quartz or calcite
Sandstone is medium-grained and is often associated with water and oil storage
Slate Metamorphic Rock
Gray rock which was originally shale
Slate has a fine-grained texture and is often used as a building material
Slate can be broken into sheets
The deeper the rock, the older the rockNicolas Steno:Steno proposed several laws that are
still important today: the principle of original horizontality the principle of lateral continuity and the law of superposition:
Assuming no change in the position of the rock layers,
The oldest rocks will be on the bottom,And the youngest rocks will be on top
He became a priest
Igneous rocks are the best for radioactive datingMany elements found
in rock may be “dated”K, Ar, Rb, Sr, U, Pb, C
In Metamorphic and Sedimentary rocks the dating only tells you when the rock was changed, not formed
There are a variety of absolute dating methods in use, most of the commonly used ones are based on natural radioactivity.
In radioactive decay an atom changes to another atom as its nucleus gives off a subatomic particle.
The starting atom is called a PARENT and the new one formed is the DAUGHTER, as P changes to D
The rate of daughter production is constant and unique for each element.
When studying a large number of parent atoms, as is usual in nature, the rate is constant.
Igneous rocks are formed from cooling molten rock
Sedimentary rocks are formed by the deposition of pieces of other rocks and the remains of living organisms
Metamorphic rocks form after exposure to heat and/or pressure for an extended time
Rock can be recycled, (the Rock Cycle)
The relative age of rock can be determined using the Principle of SuperpositionUnless the rock layers are disturbed,The layers on the bottom are oldest
Radioactive dating is used todetermine the absolute age of rocks
10. Volcanic fumes are great for your skin9. Crystal, Ruby, Opal…a bunch of names for
your daughter8. If you choose your field of research well,
you could get paid to be at the beach7. Diamonds are a girl's best friend6. Rocks rock
5. Minerals generally are very accepting and non-judgmental
4. Laugh at the people who said you'd never be a rock star
3. You can get paid to date2. "Magma" is a neat word to say. Say it with
me: "magma." See?And the number 1 reason:
1. Papa was a rollin' stone