Mathematics – Logic
Scientific paper
Apr 1985
adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=1985pggp.rept..503p&link_type=abstract
In NASA, Washington Repts. of Planetary Geol. and Geophys. Program, 1984 p 503-505 (SEE N85-23474 13-91)
Mathematics
Logic
Canyons, Escarpments, Lithology, Mars Surface, Planetary Geology, Slopes, Structural Properties (Geology), Geological Faults, Height, Morphology, Stratigraphy
Scientific paper
Throughout the Valles Marineris scarp morphology varies as a function of lithology, structure and scarp height. In addition lithology is an important control on permeability and the relative importance of spring sapping processes. Geomorphic mapping of distinct subareas can be used to define the characteristic scarp forms. Distinct morphologic zones defined on the basis of regional variations in lithology are described. Lithology and tectonic history are shown to be the two most important factors controlling slope development. Regional variation in scarp morphology can be correlated with the orientation and density of fracture systems; scarp height and the presence of rejuvenated fault scarps; and the thickness and degree of exposure of presumably less competent, more permeable, water saturated crated plateau material in the chasmata scarps.
No associations
LandOfFree
Lithologic and structural control on slope morphology in the Valles Marineris does not yet have a rating. At this time, there are no reviews or comments for this scientific paper.
If you have personal experience with Lithologic and structural control on slope morphology in the Valles Marineris, we encourage you to share that experience with our LandOfFree.com community. Your opinion is very important and Lithologic and structural control on slope morphology in the Valles Marineris will most certainly appreciate the feedback.
Profile ID: LFWR-SCP-O-1290197