AbstractUntil recently high resolution TEM was the only imaging mode capable of probing the atomic lattice structure of crystals composing tooth enamel. Studies designed to determine the polyhedral shape of normal enamel crystals and initiation of carious lesions in enamel crystals were hampered and limited by interpretation of two‐dimensional TEM images from thin section and freeze fracture replica specimens lacking depth of field. The newly developed SE‐I signal mode for SEM (SE‐I/SE‐II ratio) can produce images of enamel crystals approaching beam diameter dimensions (0.7–2.0 nm), rivaling the resolution of the TEM technique and generating topographic contrasts for three dimensional imaging at very high magnification (≈︁1,000,000 X). Ultrathin chromium (Cr) films generate enriched high resolution SE‐I contrasts of enamel crystal surfaces and when imaged using an immersion lens field emission SEM operated at high voltage (20–30 KeV) produce unsurpassed topographic contrasts. Since the grain size of Cr is below the resolution of any SEM and is ultrathin (≈︁1 nm), then SE‐I images can provide a more accurate representation of enamel crystal structure than TEM methodologies.Our SE‐I SEM observations of normal human enamel crystals reveal fractured spicules which contain angled flat surfaces delineated by a prominent 2 nm wide SE‐I edge brightness contrast. Although microscopic observations often show crystals which are hexagonal in cross‐section, in both SEM and TEM many other growth habits, including rectangular or irregular crystals (30–40 nm in width) which contain “notches,” are also observed. More detailed morphological studies are therefore required to determine the most likely habit planes and their relevance to the function of the enamel crystals. The granular appearing fine structural contrast imposed ontolattice planes of sectioned enamel in TEM micrographs is also resolved with topographic contrasts in SE‐I micrographs. These granules probably represent one