Top Banner
Homework Review Pg. 190 #1-8 , 4 ways to determine absolute age
14

Homework Review

Feb 23, 2016

Download

Documents

liko

Homework Review. Pg. 190 #1-8 , 4 ways to determine absolute age. HW pg. 190 #1-8. Why is it important for scientists to be able to determine the relative age of rocks? So that they can understand the age and history of the Earth. What events came before and after one another. - PowerPoint PPT Presentation
Welcome message from author
This document is posted to help you gain knowledge. Please leave a comment to let me know what you think about it! Share it to your friends and learn new things together.
Transcript
Page 1: Homework Review

Homework Review

Pg. 190 #1-8 , 4 ways to determine absolute age

Page 2: Homework Review

HW pg. 190 #1-81. Why is it important for scientists to be able

to determine the relative age of rocks?

So that they can understand the age and history of the Earth. What events came before and after one another.

2. State the principle of uniformitariansm in your own words.

The same processes and events have occurred throughout time in the same way.

Page 3: Homework Review

HW pg. 190 #1-83. Explain how

the law of superposition can be used to determine the relative age of sedimentary rocks.

Page 4: Homework Review

HW pg. 190 #1-84. Explain the difference between an

unconformity and a nonconformity.-An unconformity is any break in the geological record-A nonconformity is a type of unconformity where Metamorphic or igneous rock layers are covered with layers of sedimentary rock

Page 5: Homework Review

Nonconformity: part of the geological record are missing

Page 6: Homework Review

HW pg. 190 #1-85. Compare an angular unconformity

with a disconformity.

Page 7: Homework Review

HW pg. 190 #1-86. Describe how the law of crosscutting

relationships helps scientists determine the relative ages of rocks.

Page 8: Homework Review

HW pg. 190 #1-87. Which would be more difficult to

recognize: a nonconformity or a disconformity? Explain your answer.

A disconformity would be harder because it has horizontal layers of sedimentary rock on both sides of the boundary. A nonconformity can be identified by the presence of metamorphic or igneous rock below the unconformity

Page 9: Homework Review

HW pg. 190 #1-88. Crosscutting relationships.

Page 10: Homework Review

HW. 4 ways to determine absolute age of rock formations

Rates of erosion

• study erosion rates today (principle of uniformitarianism), should be similar to past rates

•for newer formations (past 10,000-20,000 years)

Rates of deposition

•average about 30 cm of sedimentary rock deposited over 1,000 years

• not all sediments deposited at an average rate (e.g. storms)

Page 11: Homework Review
Page 12: Homework Review
Page 13: Homework Review

HW. 4 ways to determine absolute age of rock formationsVarve count: annual layers can be counted

Usually form in glacial lakesCoarse summer layer covered by fine winter layer

Page 14: Homework Review

HW. 4 ways to determine absolute age of rock formations

Radiometric dating. Use the known rate of radioactive decay to estimate age of rocks by their composition

• decomposition of isotopes of an element