Planetary Geology pdf - NASA
Planetary Geology pdf - NASA
Planetary Geology pdf - NASA
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1. Sketch of cone<br />
2. Answers will vary, depending on fan speed<br />
and material (sugar or sand) used. Usually<br />
travels entire distance of table and beyond (a<br />
meter or more).<br />
3. Answers will vary, but may see a sheet of<br />
sugar/sand with ripple-like features developing<br />
perpendicular to the wind direction.<br />
4. Answers will vary, depending on fan speed<br />
and material used. Usually 1/3 to 1/2 meter<br />
for the initial bounce. The second one is shorter<br />
(less energy).<br />
5. Answers will vary, depending on fan speed<br />
and material used. Usually a few centimeters.<br />
6. Sketch (NOTE: sketches are not provided<br />
within this answer key, as the variation in fan<br />
velocities will control the speed of erosion and<br />
deposition).<br />
7. Sketch<br />
8. Erosion occurs at the front and sides of the<br />
cone.<br />
9. Deposition occurs behind the cone.<br />
10. The sketch below represents the aerodynamic<br />
characteristics of a crater when wind blows<br />
across it from left to right. Experiments to<br />
visualize this model were done at the <strong>NASA</strong><br />
Ames Research Center. For a cone, the reverse<br />
flow (seen within the crater) does not occur.<br />
11. Sketch<br />
Point of<br />
Attachment<br />
Exercise Nine: Aeolian Processes<br />
Reverse Flow<br />
Reverse Flow<br />
Answer Key<br />
105<br />
12. Depending on the shape and positioning of the<br />
obstacles, sugar will initially pile up against<br />
the obstacle (on the front and sides), some<br />
sugar will also be deposited behind each<br />
obstacle. With time the sugar will be removed<br />
from the front and sides, but will remain in the<br />
lee of (behind) each obstacle. For discussion,<br />
talk about windbreaks, such as snow fences,<br />
and other obstacles man puts in the path of the<br />
wind to control drifting sand and snow.<br />
13. Sketch<br />
14. Sketches, see answer 10 above for wind movement<br />
arrows.<br />
15. Students should see sugar within the crater<br />
moving from the back of the crater towards the<br />
front (reverse flow). Once the back rim of the<br />
crater has been removed by erosion this<br />
motion will decrease dramatically and may<br />
not be observed by the student.<br />
16. Sketches, see answer 10 above for wind movement<br />
arrows.<br />
17. Answers will vary, should be the same for both<br />
crater shapes.<br />
18. a. Answers will vary, but should have produced<br />
something similar to the windstreaks<br />
seen in the figure (most likely during Part<br />
Two).<br />
b. The average prevailing wind has come from<br />
the east (from right to left).<br />
c. The bright crater tails are most likely depositional<br />
zones of bright surface materials.<br />
Shadow Zone<br />
Vortex Core<br />
Deposition<br />
EG-1998-03-109-HQ Activities in <strong>Planetary</strong> <strong>Geology</strong> for the Physical and Earth Sciences