Syllabus
Separate lecture and lab.
Mineral Gallery
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Smithsonian Dynamic Planet
Useful Figures
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--Albert Einstein
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ATTENTION
Final Lab Exam Review
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Lecture 1
Lecture 2
Weekend Homework, Sign Sheet, Picture/Bio
Lecture 3
Lecture 4
Lecture 5
Lecture 6
Lecture 6b
Lecture 7 - The End of Sed, Beginning of Change
Lecture 8 - Skimming the Surface to Discover the Interior
Lecture 9 - A 100-yr old Eureka Moment
Exam 1 Review Sheet
Short Story Bonus Opportunity
Lecture 10 - Plate Tectonics (p1)
Lecture 10 - Plate Tectonics (p2) (plus some extra slides on how plate tectonics may start)
Lecture 11 - Streams (we didn't have this lecture - SANDBOX - but this is a good summary)
Lecture 12 - Groundwater
Lecture 13 - Waves, Beaches, Coasts
Exam 2 Review Sheet
Lecture 14 - Coasts, Relative Dating 1
Lecture 15 - Relative Dating 2
Relative Dating In-class Exercise Answer
Lecture 16 - Absolute Dating
Lecture 17 - Deformation
Lecture 18 - Mass Wasting
Lecture 19 - MSH
Lecture 20 - Earthquakes and Tsunami, part 1
Lecture 21 - Tsunami part 2 and Seafloor (plus extra)
Useful Figures
- Topographic Maps Help Sheet
- This help sheet discusses Latitude and Longitude and provides overall guidance for the lab.
- Structure of the Earth
- Details the layers of both strength and chemistry, the depths at which layer separations occur, and the thicknesses of the types of crust.
- Anatomy of a Stream
- Last slides of stream transport lecture in BIG form.
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- Common Metamorphic Rocks
- Once you figure out rock type (gneiss, etc.), typical minerals and textures, then you can ID the protolith (parent rock) and then from there you can get the facies (P and T conditions).
- Bowen's Reaction Series
- Created by N. L. Bowen, this curve will tell you the order in which minerals should crystallize. Remember, the left side is the discontinuous reaction series and the right is the continuous reaction series.
- Facies Diagram: Pressure-Temperature-Depth
- The regions tell the facies, and the P and T can be read off the diagram. On the diagram you see three words I have written. Those are the regions of stability (where you will find) kyanite, sillimanite, and andalusite. Above the minimum curve for melting, metamorphism CAN change to igneous processes (since metamorphism means change within the solid state and when liquid is involved, this is now the domain of igneous processes).
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