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FINAL STUDY GUIDE
Make sure you listen to the answers
1. DEFINE ORGANIC AND INORGANIC
Organic: Made from living things
Inorganic: Not made from living things
2. WHAT ARE THE PROPERTIES OF MINERALS?
1. Naturally formed/occuring
2. Inorganic
3. Solid
4. Definite crystal structure
5. Definite chemical composition
3. HOW ARE IGNEOUS ROCKS FORMED? EXPLAIN THE DIFFERENCES BETWEEN INTRUSIVE AND EXTRUSIVE?
Heating and cooling Intrusive: inside, coarse grained slow cooling, large crystals, lava granite
Exstruve: outside, fine grained, fast cooling, small crystals, magma, obsidian
IGNEOUS ROCKSCoarse-Grained
Fine-Grained
Granite
Gabbro Basalt
Rhyolite
4. HOW AND WHERE ARE METAMORPHIC ROCKS FORMED? FOLIATED VS. NON-FOLIATED
Heat and Pressure. Found near plate boundaries
Foliated: banded
Nonfoliated: not banded
Meta=changeMorphic=form/
shape
5. HOW AND WHERE ARE SEDIMENTARY ROCKS FORMED.
Formed by Lithification and WEDCC.
1. Weathering 2. Erosion
3. Deposition4. Compaction
5. Cementation
a. Weathering – the breakdown of material at the Earth’s surface.g
i. The weathered material is
calledSEDIMENT.
ii. Sediment size varies – mud, sand,
gravel
b. Erosion – movement of sediment from on place to another by WIND, WATER, or ICE.
c. Deposition – dropping off the sediment in a new location.
Deposition of the Mississippi
Now it’s time to put them together!
d. Compaction (Squeezing)
e. Cementation (Gluing)
5 CONTINUED
1. Clastic: made from sedimentShale (clay)Conglomerate (gravel)Sandstone (sand2. Organic: made from living thingsChalkLimestone3. Chemical: Chemical reactionRock salt (water evaporating)
i. Sand becomes sandstone
ii. Clay and mud become shale
iii. Gravel becomes conglomerate.
Organic sedimentary rock is formed from previously living things.
i. Limestone – ocean life
ii. Coal – plant life on land
Chemical sedimentary rock is formed from a chemical reaction such as
water evaporating and leaving rocks behind.
6. EXPLAIN THE ROCK CYCLE
No start and no finish
Any rock can be made into another rock if it’s FORMED a certain way
PALEONTOLOGY
7. EXPLAIN EACH LAW
1. Superposition: older rocks on the bottom and younger on top
2. Horizontality: Layers are horizontal if not disturbed
3. Uniformitariansm: The same processes that are happening now have been happening for a long time
Younger rocks are on the top.
Older rocks are on the bottom.
Layers must be undisturbed
Superposition
Uniformitarianism – the idea that the same geologic processes shaping the Earth today have
been at work throughout Earth’s history
The principle of original horizontality means that layers of sediment are generally deposited in a
horizontal position.
8 PART 1 . ABSOLUTE
Older than 50,000 = Uranium lead Method
Younger than 50,000 = Carbon-14 Method
8 PART 1 . ABSOLUTE
Most precise Gives an actual agePuts a number to the age. This is why we use it!
Uses: Radioactive decayCarbon 14 or uranium lead Half-life
8 PART 2 . RELATIVE
Sequence Age COMPARED to other rocksOlder or younger NO NUMBERUses:Index fossilsLaw of superpositionLaw of original horizontality
9. WHAT DOES THE FOSSIL RECORD TELL US?
Geological changes such as dry areas that were once under water
Organisms have become more complex and how they have evolved
How the environment looked in the past How rock layers in different areas match
up How environment/animals have changed The age of certain layers of rocks
10. WHY ARE FOSSIL RECORDS INCOMPLETE?
Most organisms don’t become fossils
11. HOW OLD IS THE EARTH
About 4.6 billion years old
12. IN WHAT TYPE OF ROCK ARE MOST FOSSILS FOUND?
Sedimentary