15.12.2012 Views

Planetary Geology pdf - NASA

Planetary Geology pdf - NASA

Planetary Geology pdf - NASA

SHOW MORE
SHOW LESS

Create successful ePaper yourself

Turn your PDF publications into a flip-book with our unique Google optimized e-Paper software.

Answer Key<br />

Map after 1) Scott et al., 1981, Map Showing Lava Flows in the Southeast Part of the Memnonia<br />

Quadrangle of Mars, USGS Map I-1271 and 2) Craddock and Greeley, 1994, Geologic Map of the MTM -<br />

20147 Quadrangle, Mangala Valles Region of Mars, USGS Map I-2310.<br />

Geologic History<br />

Unit Name Observation Interpretation<br />

A<br />

B<br />

C<br />

D<br />

flat, generally featureless plains,<br />

uniform albedo, contains faults<br />

(graben) and ridges in some areas<br />

mottled albedo, flow appearance,<br />

lobate margins, some channels<br />

evident, forms broad lobes and<br />

sheets, embays older terrain<br />

fresh craters with complete rims<br />

and identifiable ejecta deposits<br />

rugged plains, relatively heavily<br />

cratered, topographically higher<br />

than surroundings, contains faults<br />

(graben) and ridges, embayed by<br />

younger units<br />

E streamlined channel deposits<br />

Geologic Unit Structural Event<br />

Youngest<br />

C Graben?<br />

A Graben?<br />

B/E Ridges?<br />

Oldest<br />

Oldest D Tectonics?<br />

The history of this area begins with the formation<br />

of the rugged plains (Unit D). This unit has<br />

been extensively cratered. Tectonic events may<br />

have initiated at this time. Graben in the area trend<br />

216<br />

probable volcanic flows, may<br />

be mantled by wind deposited<br />

materials<br />

volcanic flows, no source visible<br />

in area<br />

impact craters<br />

old terrain of unknown origin,<br />

possibly volcanic, has<br />

undergone extensive cratering<br />

water eroded topography and<br />

fluvial deposits<br />

ENE, while ridges trend NS. Tectonic activity may<br />

have been intermittent or somewhat continuous<br />

over time, as graben and a few ridges are found on<br />

all units, but are most common on Unit D. Volcanic<br />

plains (Unit B) were emplaced in the eastern section<br />

of the mapped area; the source of these flows<br />

is not contained within the map area, but most likely<br />

is to the east. Fluvial activity, perhaps concurrent<br />

with volcanic flow emplacement, cut topographic<br />

features and deposited materials (Unit E) in the<br />

north-central section of the map. The age relation<br />

between units B and E is unknown. Large craters<br />

and low land areas were filled by Unit A, probably<br />

consisting of volcanic flows and a mantling<br />

dust/sand deposit. Finally, impacts occurred forming<br />

the young craters and their ejecta blankets.<br />

Exercise Seventeen:<br />

Photogeologic Mapping of Mars<br />

Activities in <strong>Planetary</strong> <strong>Geology</strong> for the Physical and Earth Sciences EG-1998-03-109-HQ

Hooray! Your file is uploaded and ready to be published.

Saved successfully!

Ooh no, something went wrong!