Suspended matter in Astoria canyon was monitored by means of an in situ nephelometer and by means of light-scattering and particle concentration measurements performed aboard ship on water samples. Nephelometer profiles obtained along the axis of the canyon in February and April 1973 indicate that the canyon is divided into two distinct zones: a nearshore zone in which the suspensoid distribution undergoes large changes and an offshore zone in which the distribution varies to a much lesser degree. A 15-hour time series of light-scattering and particle concentration profiles at a depth of 1100 m in the canyon shows extensive and rapid changes in suspended matter concentration at several depths. The effect of nonsteady state distributions of suspended matter on calculations of the coefficient of eddy diffusivity is examined and shown to be an important consideration in a submarine canyon. The extent to which observed distributions of suspended matter vary with time is important relative to their roles as indicators of abyssal circulation and sediment dispersal, and at the present time, information on the time variability of suspended particulates, especially in the deep ocean, is limited. In estuaries and on the continental shelf a great deal of work has been done concerning the distribution and transport of sediments [Swift et al., 1972]. However, observations of changing distributions of suspended matter, which are an integral part of the problem of sediment transport, have been rare. The response of suspended sediment to tidal effects has been studied by Schubel [1969, i971], Wasowski [1974], and others. Over the cohtinental shelf, Rodolfo et al. [1971] have observed the responses of suspended matter to a hurricane, and Harlett [1972], in a study of sediment transport on the shelf off Oregon, reported several time-series measurements of light transmission in depths of 100-200 m. The data presented in this report resulted from our efforts to determine how the observed distributions of suspended particulates respond to the regimes of wind, surface and internal waves, and tides and currents in deep oceanic waters. Our initial efforts in this study were to determine .the extent in time and space of changes in the concentration of suspended matter in the nearshore region and to extend these measurements offshore. It was felt that Astoria canyon would be an advantageous site for this study for several reasons. It has been suggested often [Moore, 1969; Lyall et al., 1971] that submarine canyons are sites of 'channelization' of sediment transport and perhaps of bottom water flow, and there have been numerous studies of bottom currents in submarine canyons [Fenner et al., 1971; Shepard and Marshall, 1973; Keller et al., 1973], all of which have shown that bottom currents of significant magnitude exist in canyons and that flow reversals are common. One /