Mars and Earth: Curriculum Support Materials and Lessons on Mars Exploration by David V. Black Walden School of Liberal Arts, 2011.

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Presentation transcript:

Mars and Earth: Curriculum Support Materials and Lessons on Mars Exploration by David V. Black Walden School of Liberal Arts, 2011

Overview Three lessons that are appropriate for classes in Earth science, geology, astronomy, multimedia, or computer literacy. These materials fit into national standards for grade science. Teachers can use all or parts of the lessons and materials.

1. Mars Site Selection Introduces Martian geography. Introduces the science objectives of the Mars Science Laboratory (Curiosity). Shows how landing sites are chosen collaboratively. Teaches students to develop and defend a proposal.

2. Finding Mars on Earth Mars has an arid climate. The Great Basin of Utah and Nevada is an excellent analog for Mars. Students will use latitudes and longitudes to examine Earth and Mars analogs in Google Earth.

2. Finding Mars on Earth Students will develop hypotheses about the processes that formed each terrain, based on observations and comparisons. They will draw conclusions about the presence of long-lasting water at the sites.

2. Using Google Earth Google Earth is a freeware program. You will need to install the program, and be connected to the Internet, to use the search functions. Using the trackball and zoom controls in the upper right corner allows a 3D view of the location.

3. From Mars to Model Simulates the data collection, analysis, and modeling of the MOLA instrument on Mars Global Surveyor. Uses clay terrains in a box with a regular grid of holes in the lid.

Popsicle sticks are used to record topographical data (color-coded) and altitude measurements. Scales are reversed so that the height of the mountains, not the depth of the valleys is measured. 3. From Mars to Model

Three models are created. Model A is a direct color- coded topographical model. The color seen on the stick is painted into the squares on the paper grid. Light colors (yellow and orange) are high areas, dark colors (brown and black) are low.

Model B is a physical model. Lengths of drinking straws are cut to match the numeric data (mountain heights). These are stuck into a rolled-out layer of modeling clay or plasticine in the same grid pattern. 3. From Mars to Model

Model C is a virtual model using 3D software. Numeric data is typed in a word processor as a sequence of numbers separated by commas, with a new line for each new row. The file is saved in.txt format. 3. From Mars to Model

The.txt is opened as a text image in ImageJ. The small file is zoomed in and saved as a screen capture (Shft-Cmd-3 on Macs, PrntScrn on Windows). 3. From Mars to Model

The screen capture is loaded into GIMP (open file and locate Picture 1 for Macs, “File - Create from Clipboard” for Windows). Crop the image if needed. Increase the image resolution. 3. From Mars to Model

Change the canvas size to make the image square. Select the area outside the grayscale heightmap and fill it with black. Save the file as a high- quality.jpg. 3. From Mars to Model

Open Daz3D Bryce and create a new terrain. Open the Terrain Editor and load in the heightmap image (Step 1). Copy the image (Step 2) and paste it to the middle square (Step 3), then paste it back into the left square (Step 4). Apply the image to the terrain (Step 5). From Mars to Model

Make the terrain solid, then exit the Terrain Modeler. Add a Material to the terrain and to the ground plain. Position the camera and the sun. Render the scene and save (Export Image). 3. From Mars to Model

Increase the resolution of the model by moving the original grid by.5 cm right, then down, then left. Collect data points each time. You will have doubled your resolution and increased the data size by four times. 3. From Mars to Model

Practical Applications: In computer graphics, doubling the resolution means having four times as many pixels. As models contain more data, they resemble the real object more closely. Mars MOLA instrument built up higher resolution by offsetting its orbit and then adding the new data back in between the old.