Geology 12 - Historical Geology | |||||
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The main things we want out of this chapter are 1) the evidence for Cambrian environments and 2) the evidence severe weather leaves behind. Be sure to note the links to other Web Sites and be sure to visit them to answer the questions.
Terms you should know:
aulacogen - |
1. Breakup of the Proterozoic supercontinent
What is the evidence that at least one supercontinent existed in the Proterozoic? (we'll do this in class)
To see reconstructions of the Proterozoic supercontinent:
- Go here, click on Precambrian, then Cambrian
- For an interactive look, go here, then click and drag the cursor across the image to run the animation.
What is the evidence that a supercontinent broke up at about 500- 600 mya?
2. Cambrian rocks
What is the significance of each of these features of Lower Cambrian sandstones?
- very well rounded
- almost pure quartz
- frosted (microscopic abrasions)
- large and small scale cross-beds
What do we conclude about how these sandstones were deposited? What does it tell us about the tectonic setting of North America (and much of the world)?
How did deposition change toward the end of the Cambrian? What does this tell us about paleogeography and plate setting?
3. Episodic events
Find at least three indications of severe weather events left behind in Cambrian rocks. Why would we expect the sedimentary rocks of this large epeiric sea to be impacted primarily by large episodic storms rather than gradual deposition?
4. What was the paleoclimate of North America during the Cambrian?
What evidence exists to tell us about paleoclimate?
1. Proterozoic supercontinents
You should be able to:
2. Cambrian sediments
You should be able to:
3. Episodic events
You should be able to:
3. Paloeclimate
You should be able to: