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Published byReynard Holland Modified over 8 years ago
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Identify and label the different continents on your map. North America South America Africa Europe Asia/India Australia Antarctica
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Take 2 minutes to observe the world map. Make 2 observations about the continents’ coast lines. Make 1 inference based on your observation End
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Take 3 minutes and work with your partner to try and fit the continent puzzle pieces together. End
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Do they fit together perfectly? What may have caused the coastlines to change over time? Come up with 2 possible reasons (2 minutes) End
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Look at the small pictures on your puzzle pieces. Those are fossils found in those areas of each continent. Take 2 minutes to observe the fossil placement. Make 2 observations Make 1 inference End
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Rearrange your puzzle so that all of the fossil segments line up. (2 minutes) End
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Take 3 minutes to draw in dots along the plate boundaries to show recent earthquakes. (large dots = more activity, small dots = less activity) End
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Take 2 minutes to draw in triangles to show volcanic activity. End
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Take 2 minutes to observe the marks you just made on your map. Make 2 observations Make 1 inference End
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1. Which type of dating would you use to find the age of an ancient basket made of natural fibers? Why? 2. The element Chaparralium has a half-life of 24,000 years. If a fossil contains.195% of the original amount of Chaparralium, how many half lives have passed? How old is this fossil? Show your work!
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Alfred Wegner Concept with no mechanism
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1. The continents fit together. 2. Fossils of the same organisms are found along the coasts of different continents.
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Supercontinent 300 million years ago Cycle
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Scientific theory (concept + mechanism) Lithosphere is broken up into “tectonic plates” Moved by convection of asthenosphere Past plates and current plates How do we know? How many? Farallon Plate
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3. Seismic, volcanic, and geothermal activity along plate boundaries.
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4. Sea Floor Spreading Mid-ocean ridges Tectonic plates moving separating New magma rises Form new oceanic crust Older crust pushed away
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5. Magnetic Reversals Molten rock Magnetic minerals Align with magnetic field Magnetic field reverses 177 times in 85 million years Last 600,000 years ago Recorded in rock Similar pattern to age of rocks
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Convection Asthenosphere Heated rock Expands and rises Cools More dense
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1. Spreading New material pushed up at ridges Pushes older material away 2. Subduction Denser plate sinks Pulls rest of plate 2 main types of movement
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