Scanning electron microscopic imagery is often used to identify and discrim
inate among environments of sedimentation with the main aim of identifying
individual microfeatures, or suites of microtextures, that are considered i
ndicative of a particular depositional environment or geologic process. Bec
ause few microtextures are considered to represent a single geologic proces
s it is necessary to analyze a large number of quartz sands and other miner
alic grains with the objective of determining the frequency of occurrence o
f a range of microtextures within a distinct sample suite. Using percent fr
equency of occurrence of different microtextures from suites of fluvial, gl
aciofluvial and glacial sands from sites in Estonia and Latvia, we invoked
statistical comparison of different sample suites using Euclidean distances
. These provide a quantitative means of measuring the differences among dif
ferent sediments and processes that formed them and also a quantification t
ool useful in assessing microtextures as a recorder of sedimentary environm
ents.