Transmission electron microscopy has been applied to the study of sediments and sedimentary rocks.%6, 10 A specialized field has developed concerned with the environmental interpretation of the surfaces of quartz sand grains; and it has been possible to distinguish between recent littoral grains, recent eolian grains, glacial grains, and those subjected to weathering and the diagenetic environments.l-4,7,9,13-l~,20-23,26-28,3ly34,35,38,39 Recently the scanning electron microscope (SEM)29,30,33,36 has beenused to study the surface morphology of a large variety of objects including foraminifera and diatoms.11,32 The SEM is considerably faster than and gives more realistic photographs than the transmission electron microscope (TEM); the SEM allows the observation of a large number of grains at one time and, due to the greater detail observed, permits additional environmental information to be obtained. This paper will compare the TEM with the SEM and suggest why the latter is so much more valuable than the former in the interpretation of sand grain surface textures.The rationale behind the use of sand surface textures for environmental interpretation is indicated below. Preparation techniques for both instruments a r e discussed and the SEM is described in t e r m s of its operation and its superiority over the TEM. Criteria characteristic of the various environments a r e noted and pictured; finally, applications of the SEM technique are discussed.
RATIONALEQuartz sand grains representing known modern littoral, modern eolian, late Wisconsin glacial, and certain diagenetic environments were collected from various parts of the world and examined for characteristic surface textures. This permitted identification of textures representing known environments. Most of these textures were then duplicated experimentally.13-15,40 Older fossil sands from known environments were examined and compared with the original groups and the experimental grains. Surface *This paper, illustrated with slides, was presented at a