Week 3: The Moon, Phases, and Different Sides

 

  1. What did you do in lab today?

    1. We did an experiment looking into why the front and back sides of the moon look different and why different parts of the moon have thicker crusts than others. We got to experiment with different thicknesses of the moon's crust to see how craters are created. 

  2. What was the big question?

    1. Why does the moon have two very different-looking sides? 

  3. What did you learn in Thursday’s discussion?

    1. Earth facing side of the Moon is 200 degrees warmer 

    2. There is gravity on the moon, but it is just a lot less than there is on Earth 

    3. There are many different theories on how the moon was created 

    4. The moon is in its new moon phase just before and after a solar eclipse 

    5. The moon is about the size of the United States 

  4. Read chapter 3 of the online textbook.

    1. What did you learn?

      1. I learned that the moon has craters because it lacks an atmosphere to protect it from impact, and there is no weather to erode the craters away. I also learned that the Moon’s gravity causes tides in the ocean. I have been to the ocean multiple times, and I never knew what caused high tide and low tide. 

    2. What was the most helpful?

      1. I found the image that shows the position of the Moon, Earth, and Sun during all the different moon phases very helpful. I am a visual learner, so this was helpful in showing me where each of these is instead of someone just telling me. We talked about moon phases in lab today, which emphasized the different positions for each phase. 

    3. What do you need more information on?

      1. I do not need any more information on anything from the textbook. I think this chapter was very well written and provided a lot of details and information about what we talked about in this week's lab. 

  5. What questions, concerns, and/or comments do you have?

    1. I do not have any questions, concerns, and/or comments after this week’s lecture and lab.

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