An examination of 189 well-delineated mounds and pits in sandy soils o
f northern lower Michigan, all presumably formed by tree uprooting, wa
s used to determine the effects of slope angle on morphology and volum
e, and to assess the potential importance of uprooting to mass movemen
t. Slopes ranged from zero to 54%. Data indicate that mound and pit vo
lumes increase with increasing slope angle, suggesting that on gentle
slopes more of the disturbed soil wastes off the mound, back into the
new pit. Mounds are often elongated in the downslope direction on stee
p slopes. Based on regression analyses, slopes of approximate to 47 de
grees are generally sufficient for all mound soil to slump or wash off
in a downslope direction, rather than into the upslope pit. Thus, on
steep slopes pit volumes provide a better representation of root plate
volume. Pit depth can also be used as a surrogate for rooting depth o
n steep slopes where infilling from the mound is minimal.