CONSTRAINTS on THE SURFACE EVOLUTION OF VENUS GLEANED FROM MULTIPLE DATASETS: IS CATASTROPHIC RESURFACING VIABLE?
A variety of geologic and surface modeling studies provide robust constraints for surface evolution hypotheses. These studies include: a) Monte Carlo crater modeling; b) impact crater characteristics, evolution and relative ages; c) ancient ribbon-tessera terrain character, distribution, and history; d) radial dike swarm characteristics, global distribution, and temporal constraints; e) global and regional wrinkle ridge patterns, and the relative ages of wrinkle ridge suites; f) the age of volcanic plains units relative to adjacent features; g) the nature and distribution of shield terrain; h) the surface expression and evolution of Artemis, a monstrous circular feature with two concentric troughs (2400 and >5000 km diameter), a radial dike swarm (12,000 km diameter), and concentric wrinkle ridges (13,000 km diameter); i) the characteristics and relative ages of crustal plateaus and volcanic rises; and j) constraints derived from geologic mapping of numerous VMap regions (~7.5x106 km2 each) by independent workers, which eliminates the need for a singular resurfacing event.