Jm. Kabrick et al., CRADLE-KNOLL PATTERNS AND CHARACTERISTICS ON DRUMLINS IN NORTHEASTERNWISCONSIN, Soil Science Society of America journal, 61(2), 1997, pp. 595-603
Cradle-knell microtopography has been shown to influence soil and vege
tation. However, the scale of commonly used topographic maps is too co
arse for representation of microtopography. The objectives of this stu
dy were to investigate the influence of cradle-knell microtopography o
n the distribution of trees, to develop a method to quantify the spati
al patterns and characteristics of cradle-knolls, and to test for patt
ern similarity of cradle-knells within and among drumlins in the Nicol
et National Forest, Wisconsin. Six drumlins were selected for study. T
ree species, tree diameter, and microsite location (e.g., cradle, knel
l, or neither) within which each tree was found were inventoried in th
ree, 10-m-radius plots across each drumlin. The spatial location, leng
th, width, relief, and orientation of 220 cradle-knells were inventori
ed along 200-m transects using a T-square sampling technique on summit
and backslope positions of each drumlin. Sixty percent of the trees i
nventoried were growing on knells and only 2% were growing in cradles.
The same number of knells and cradles occurred among drumlins and amo
ng backslopes and summits within drumlins. Cradle-knell relief differe
d among drumlins, and knell relief is greater on backslopes than on su
mmits within drumlins. Cradle-knell orientation differed among slope p
ositions. These findings suggest that treethrow rates and the size of
the uprooted trees are roughly the same among and within drumlins. Dif
ferences in relief among drumlins are probably an indication of how re
cently treethrow has occurred. Greater relief of knells among backslop
es and summits is probably because of slope-mediated differences in cr
adle-knell formation. Slope position also affects cradle-knell orienta
tion in these landscapes.