Pair instruction: (please find file attached ) please fill in the template and
Given the attention that has been accorded to the need to prepare and present experiences for participants that are both effective and inclusive, it is important that the pair task reflects your critical awareness of the ‘isms’ we have explored. In other words, it should focus on more than just learning how to move well, play sports and games or get fit.

In pairs you are required to develop a learning opportunity for your tutorial group. This learning opportunity must demonstrate your understanding of how the topics covered this semester can be enacted at an applied level. You will also need to consider what pedagogical strategies (the nuts and bolts of managing the learning environment) you will need to employ to ensure your learning opportunity is engaging for all learners and runs smoothly.

You will have a maximum of 15 minutes to run your learning opportunity. There will be a five minute transition time to allow a pair to set up – no longer! The week and order for your practical will be determined in tutorials.

 

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Plate tectonics is a unifying framework for understanding the dynamic geology of the Earth. The theory posits that the outermost layers of the Earth (the crust and uppermost mantle) make up the brittle lithosphere of the Earth. The lithosphere is broken up into a number of thin plates, which move on top of the asthenosphere (middle mantle). The asthenosphere is solid, but flows plastically over geologic time scales. Plate interiors are relatively stable, and most of the tectonic action (earthquakes, volcanism) takes place where plates meet – where they collide at convergent boundaries, move away from one another at divergent boundaries, or slide past one another at transform boundaries.

Reconstructions of the Earth’s tectonic plate locations through time are available, for example, at:

http://www.scotese.com/newpage13.htm

(Links to an external site.)

http://www.ucmp.berkeley.edu/geology/tectonics.html

(Links to an external site.)

But how do we define plates and plate boundaries? On what are plate reconstructions and animations based? How do we know plates are moving, how can we track their positions in the past, and how can we predict their positions in the future?

To answer these questions, this assignment guides you through an examination of patterns on Earth – the topography of the earth’s surface above sea level, the bathymetry of the ocean floor below sea level, and the distribution of earthquakes and volcanic rock ages. These patterns reveal plate boundaries, just as they did for geologists first developing plate tectonic theory in the 1960s. You’ll then use geologic data to determine long-term average plate motions, to predict how our dynamic planet will change in the future.

To do this, you’ll use the program Google Earth, and Google Earth layers compiled from various sources.

 

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introduction to plate tectonics with google earth 2 was first posted on July 14, 2020 at 10:15 am.
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introduction to plate tectonics with google earth 2 was first posted on July 14, 2020 at 10:20 am.
©2019 "Essay Lords | Bringing Excellence to students world wide". Use of this feed is for personal non-commercial use only. If you are not reading this article in your feed reader, then the site is guilty of copyright infringement. Please contact me at support@academicheroes

 

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