Mercury

General Characteristics


Surface

Craters


Inter-Crater Terrain


Scarps

cliffs
curved, cut some craters;
other craters cut scarp.

- interpreted as thrust faults

- indicate compression (global shrinkage) over long time periods, occurred near end of bombardment phase, one tenth of 1% crustal shortening.

- not seen any other place except Earth & perhaps Ganymede.

- probably formed during cooling & contraction of planet
(heated to melting point during bombardment)

- during cooling, bombardment caused large flat craters

Mercury cooled more slowly than Moon due to its larger size.

- surface of Mercury may be younger than Moon's
more craters due to higher gravity.


Future Exploration

February 21, 1996