|
Be sure to know the following:
- The three Martian eras, their sequence, rough time ranges, and main
areological events
- Landscapes associated with the three different eras
- Crater density and size distribution as a key to dating Martian surfaces
- Why water vaporization can lead to the loss of water (perhaps even an
ocean's worth) from Mars
- Comparison and contrast between "Mars Attacks!" (1996) and "War of the
Worlds" (1953)
- Dominant water and carbon dioxide fluxes and Martian seasonality
- Vertical structure of the Martian atmosphere by the relationship between
air temperatures and altitude
- Vertical structure of the atmosphere by the degree of mixing and of
gravitational gas segregation
- Gaseous composition of the Martian atmosphere: Main gasses (say, top
four)
- Why is nitrogen's isotope ratio of such interest in understanding the
potential for a wet early Mars?
- The Martian "geographic grid" -- the most common system used today with +
and - for north and south and 360° of longitude, running east -- be able
to convert between the Earth system and the Mars system
- Characteristics of the main Martian regions, including their locations:
- The great crustal dichotomy and the elevation, age, and rock-type
differences between the northern third and the southern two-thirds
-
Valles Marineris and its subsidiary chasmata (including their locations
with respect to one another) and Noctis Labyrinthus
- Tharsis and its five main volcanoes
- Elysium and its three main volcanoes
- Thaumasia Montes and why this feature is not like other montes on Mars
- evidence for and against plate tectonics on Mars
- the polar ice caps and their similarities and differences in chemical
composition
- patterned ground (polygons) and its possible connection with permafrost
- evidence for glaciation at relatively low latitudes in and around the
Elysium Montes
- why might sapping alcoves/channels/aprons evidencing liquid flow be found
on poleward-facing slopes at high latitudes?
- possible explanations for chaos terrain
- the main impact basins: Hellas, Argyre, Isidis, Utopia
- through which evidence is it argued that the Hellas Planitia impact
struck at the very end of the Noachian era?
- Vastitas Borealis and evidences for and against a Noachian ocean
- Noachian landscapes: Noachis Terra, Arabia Terra, and Terra Sirenum
- Hesperian landscapes: Hesperia Planum, Terra Tyrrhena, Aonia Terra,
Margaritifer Terra, Syrtis Major
- Amazonian landscapes: Amazonis Planitia, Utopia Planitia, Chryse
Planitia, Acidalia Planitia
- Know the main types of landforms on Mars and the planetary gazetteer name
for them (there's a table in my lecture notes)
- Be able to idenfity and differentiate various channel systems: possible
dendritic fluvial valles (that look like Earth precipitation-fed channelized
surface flow networks), sapping-fed systems, channels linking craters that may
have had lakes in them, and the massive outflow channel systems that look like
Earth's jökulhlaup features
- Know the main Martian weather features and the locations and seasons you
can expect them (polar cyclones, dust devils/dust storms, mid-latitude wave
systems, thermal tides, upslope-downslope breeze/wind systems) and how
atmospheric clarity/dustiness affects them
- Be able to read the water phase diagram (it's in the Fourth Order
viewgraphs, the X-Y graph showing the triple-point of water) to predict,
generally, how water will behave in different temperature and pressure
conditions
- Be able to look at a complex terrain on Mars and pick out some of the
processes that might explain its many features
- Evidences for lakes in the southern highland craters
Tips:
- Do all the reading
- Make use of those map study guides, which I'll be collecting during the
final
- Avail yourself of my lecture notes, which I put online and accessible
from the home page: http://www.csulb.edu/~rodrigue/mars/
- I have put a link to that MOLA map that I labeled with lots of useful
place names
- Make use of the viewgraphs: The final covers "Mars Planetary Basics"
through to "Fourth Order of Relief"
- Read your colleagues' web efforts: I have taken one question from each
of them
- The final is open everything, but you need to be familiar enough with
everything to be able to find it when you're freaking out
- Studying with your colleagues is highly recommended: You can get hold of
them to schedule a review session through BeachBoard, also linked to the
course home page.
|
|