As technology advances, the way in which geologists study the Earth also advances. Some of these new technologies also make it possible to bring aspects of the field into the classroom. This opens up opportunities for broader audiences to explore a wider range of geologic structures and localities. Structure from motion (SfM) is one of these technologies that is
Exploration of the Antarctic continent did not occur until the late 1800’s, and the South Pole was first reached on December 14, 1911. Courage, planning, and technology have been the main components of Antarctic exploration from the earliest days. This classroom activity is designed to highlight the historical elements of the past 100 years of exploration in Antarctica and
Small groups of students will establish their own phenology plots for long term study. Students will make a field sketch of a sample plot and turn it into a scale map. The map will accurately place plants the students have identified for tracking phenophases, so that the plots can be monitored long term. Phenology is a vital part of
Students will conduct a soil study by investigating pH and water absorption.
Objectives
Students will learn:
* How to describe the composition of soil and explain how it forms.
* That soil is made up of tiny particles of rock, plant, and animal matter.
* How to determine whether a solution is acidic, basic, or neutral.
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Students will investigate what a carbon footprint is and calculate their own personal carbon footprint. Finally, students will develop ways to reduce their carbon footprint.
Objectives
Students will know that the principles of chemistry underlie the functioning of biological systems.
Students will know that carbon, because of its ability to combine in many ways with
Powerpoint presentation given at 2012 North Carolina Science Teachers Association professional development conference "Catch the Wave". Co-presenters Nick LaFave and Susan Steiner presented their PolarTREC experiences and information about PolarTREC.