Hypsometric topographic analysis of Magellan altimetry data at Alpha R
egio results in a multimodal distribution. Planimetric display of the
spatial distribution for altitudes close to each mode reveals large-sc
ale ring-like and crescentic patterns. The latter result from the inte
rsection of horizontal altitude ranges with sloping patterns that are
quasicircular in shape. The spatial patterns of topographic features n
ear Alpha Regio have the following attributes: (1) quasicircular shape
s of individual elements; (2) a hierarchy of distinctive sizes for tho
se elements, with diameters of various elements at approximately 2800,
1500, 500-700, and 200 km; and (3) a large-scale arrangement or patte
rn in which the 1500-km highland plateau of Alpha Regio is surrounded
by a ring of 500-km structures, all of which constitute a 2800-km mega
structure. We hypothesize that the intricate patterns of hierarchical
scaling for large-scale spatial elements of Venusian topography result
from corresponding complexity in Venusian mantle convection.