Earth Systems and Sustainability Dr. Debrah Fine La Jolla Country Day School Study Guide for Trimester 2: Test 1 The first test of the trimester is on Wednesday or Thursday, January 23nd/ 24th, 2013. We will review in class on Friday, January 18th and Tuesday, January 22nd. I will be available for extra help on Tuesday January 22nd after school. Here is a list of items you should review: Review the last quiz: Review your mistakes on the last quiz. Much of the material on the quiz is essential for understanding the material that followed. Review your study procedure for the last quiz and make any necessary adjustments. Remember to: Use flashcards Study with a friend and explain things to each other Start your studying early and ask questions if needed Readings and Homework Questions: The readings are all called “Digging Deeper” and the questions are the “Check Your Understanding” questions on the side of the page. These were handed out in class, but you can download them on the class website as well. The date below matches the date the homework was assigned. 2012-12-17: 2012-12-17: 2013-01-07: 2013-01-08: 2013-01-14: 2013-01-15: An Earthquake in Your Community How Big Was It? An Earthquake History of Your Community Ring of Fire Student Guide and Questions Lessening Earthquake Damage Mystery of the Far Flung Fossils: Investigating Plate Tectonics Activities: 1. Ring of Fire Activity: Understanding the relationship between plate tectonics and geological features, volcanoes, and earthquakes. 2. Mystery of the Far Flung Fossils: Investigating Plate Tectonics Notes: Review your notes from class including homework corrections. Videos 1. Evidence for Pangaea (concept also covered in readings and activities): https://www.khanacademy.org/science/cosmology-and-astronomy/earth-historytopic/plate-techtonics/v/pangaea 2 Study Guide Last Quiz: Lithosphere versus asthenosphere Convection currents in the asthenosphere driving plate motion How density differences drive convection currents Density, mass, and volume calculations Types of plate boundaries: o Divergent o Convergent o Transform Types of convergent plate boundaries: o Ocean-ocean convergence o Ocean-continent convergence o Continent-continent collision Geological features associated with the different types of convergent plate boundaries: o Ocean-ocean convergence: subduction occurs resulting in a trench and volcanoes (volcanoes become volcanic islands) Example: Aleutian Islands off the coast of Alaska o Ocean-continent convergence: subduction occurs resulting in a trench and volcanoes (volcanoes become volcanic mountain arcs) Example: Andes Mountains in South America o Continent-continent collision: no subduction occurs due to low density of continental crust. Collision results in mountains. Example: Himalayan Mountains (e.g. Mount Everest) ***YOU SHOULD KNOW THAT PLATES WITH CONTINENTAL CRUST ON TOP DO NOT SUBDUCT BECAUSE THEY ARE NOT DENSE ENOUGH TO SINK INTO THE ASTHENOSHPERE*** Material Since Last Quiz Earthquakes: o Scientific definition and cause of earthquakes o Focus versus epicenter o Types of plate boundaries and which ones lead to earthquakes o Magnitude versus intensity o Distribution of earthquakes and how this supports the theory of plate tectonics o Earthquake damage (primary hazards, secondary hazards). o Types of seismic waves and differences between them Earth Systems and Sustainability Dr. Debrah Fine La Jolla Country Day School Ring of Fire Mapping activity: Ring of Fire: o What is it? o What plate does it surround? Alfred Wegener’s Theory of Continental Drift o What kinds of data did Alfred Wegener use to develop his Theory of Continental Drift? o Why didn’t other scientists believe him? o How is the Theory of Continental Drift different than the Theory of Plate Tectonics? Mystery of the Far Flung Fossils Activity: Understand how the Theory of Plate Tectonics is supported by fossil evidence and be able to determine which continents were connected at a certain time based on the fossils present at that time. Be able to identify the pieces of evidence that support the Theories of Continental Drift and Plate Tectonics o Fossil evidence (continents that were connected had similar fossils from the same time period) o Glacial grooves (advancing glaciers carved grooves into the continents and the pattern only makes sense when the continents are all connected into one land mass) o Mammals evolved independently (there are very different mammals on the different continents and mammals evolved after the continents had moved apart, so the differences we see in modern mammals supports these theories) o Closely related species exist on continents that were previously connected (which suggests that they shared a common ancestor when the continents were connected and then evolved to survive in the differing conditions on the continents after they drifted apart). o Shape (the continents fit together like puzzle pieces) o Global positioning system (GPS) data (confirms that the continents/plates are in fact moving, and if you “rewind” this movement, the continents move back together into one land mass)