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Scientific Question | MARS Project Application Form | Lesson Plans and Teacher Resources

Did it ever rain on Mars?


This is the question we need your help to answer! Were the valley networks on Mars carved by sapping or run-off?

Color Mars Image Black and White Mars Image
Valley network on Mars
(source: http://www.solarviews.com/cap/mars/network.htm )
copyright by Calvin J. Hamilton used with permission
Dendritic drainage pattern in Yemen
(space shuttle photograph)
(Source: http://www.solarviews.com/cap/earth/yemen.htm )


MARS Project Application Form

Registered users, click here to enter your Mars section(s).

New teachers or teachers who wish to sign up for additional sections please click here.


Lesson Plans and Teacher Resources

Here are lesson plans, PowerPoints and other materials that go along with the web-GIS lessons. These lessons are standards-based. (See the Introduction for the listing of the specific standards.) The lesson plans are inquiry-based and target grades 8-10 but can be expanded to grade 14. The lessons introduce the basic geologic concepts necessary to be able to understand run-off and sapping and to be able to use this knowledge to evaluate whether their section of Mars is typical of run-off (rain likely) or sapping (rain unlikely).

The modules include embedded tutorials but an overall tutorial may be found here or by clicking the tutorial main menu item.

Module 1:  This lesson serves as the introduction to the MARS EPO project. The goal of the MARS EPO project is to promote inquiry-based learning to analyze actual NASA data in a web-GIS program to answer the question, “Did it rain on Mars?”  The Martian surface is covered by numerous valley networks that could have been formed by either (a) groundwater sapping or (b) surface run-off.  This lesson is designed to introduce the concepts of groundwater sapping and surface run-off to the students through the use of a stream table.  The second day of this lesson also provides students the opportunity to begin working with the web-GIS website to identify amphitheater heads, a major characteristic of groundwater sapping.



Module 2:  This lesson introduces Mars as a planet to the students. During the course of the lesson the students will  list the main similarities and differences between the planets Earth and Mars, hypothesize on why Mars is called the Red Planet and what that has to do with whether it ever rained on Mars and use the web-GIS software to begin to answer the question whether it ever rained on Mars.



Module 3: 
As students begin to investigate the Martian surface, they will see that numerous channels cover it.  In this lesson, students will first learn how to identity different stream drainage patterns in map view through the use of a worksheet and a PowerPoint presentation. Students will then, through the use of the PowerPoint presentation and a sample problem, gain understanding of drainage basins and drainage density. They will practice by determining the drainage density of two simplified drainage systems on paper followed by using the web-GIS software on their sections.



Module 4:  As students learn about the many types of geological landform features, such as hills, mountains, valleys and watershed drainage basins, it is important that they have some understanding of hypsometric curves and circularity functions and why they are useful to geoscientists. The students will use potato models, produce hypsometric curves and circularity graphs and determine whether the drainage basin represented by the carved potatoes are more consistent with run-off or sapping. They will apply this knowledge to the actual Martian database and determine whether the watersheds in their assigned area are more likely due to run-off or sapping processes.


Final Report:  This is the form the students fill out at the end of their analysis. This is where they document their discoveries and make their argument as to whether they believed it has ever rained on Mars. The final reports of all sections will be downloadable for all participating groups.



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