We have investigated size distribution of rampart craters in the east
edge of Chryse Planitia on Mars by Viking high resolution images. Clea
r existence of the onset diameter of rampart crater, which defines the
minimum size of the rampart crater, has been recognized. If this diam
eter corresponds to the depth to the top of the volatile layer, the co
nverted depth ranges from similar to 20 m to 60 m. These values are sy
stematically shallower than the previous estimates (Kuzmin, 1988). Mar
tian volatile layer is thought as a main reservoir of the ancient fluv
ial processes and atmospheric water vapor. This shallow volatile layer
gives us information of the inventory of Martian water and conditions
of cryosphere.