The geomorphological description of the Lower Mississippi Valley (LMV)
as presented by Harold N. Fisk in 1944 differed from most other repre
sentations in that morphogenesis was always implied. The intellectual
climate of the times was highly conducive to the multidisciplinary app
roach. Then archaeologists were accepting the premise that the cultura
l history of the New World involved a few millennia rather than just s
everal dozen centuries. It is fortunate that some of the most active a
rchaeologists came on the scene with strong backgrounds in geology and
related earth sciences. These prehistorians were sensitive to the rol
e of the environment in shaping the relationships of man and land. Vir
tually every archaeologist who worked in the LMV immediately came to r
espect and utilize the concepts of Fisk. Because, in part, to the intr
oduction of radiocarbon dating, archaeologists of the last half centur
y have furthered the refinement of Fisk's chronology but the basic con
cepts have remained. This is not to say that there have not been vigor
ous challenges to Fisk, but they have not destroyed the usefulness of
this monumental contribution.