The available data on the terrestrial influx of small meteoric particles (mass <• I gram) are surveyed. Whereas, in the past, flux determinations differed by factors of as much as 100 million, it is shown that recent experimental data are far more consistent, variations being limited to a factor of 10 for particles of mass greater than 10 -•ø gram. The sensors from which the data are obtained are discussed, with particular emphasis on those used in situ, and inherent uncertainties in the results are pointed out. A best estimate of the cumulative mass distribution influx is given on the basis of the most recent data available. This estimate uses the NASA Meteoroid Environment Model, 1969•. Uncertainty limits due to differing experimental results and interpretations are placed upon this flux model. For masses larger than about 10 -•ø gram, the uncertainty is less than I order of magnitude; whereas, for smaller particles the uncertainty may still be as large as 4 or 5 orders of magnitude. The present best estimate of the mean density of the small meteoric particles is 0.5, g/cm s, but there are indications that several classes of meteoroids exist with densities ranging from 0.3 to 1.2 g/cm s.The importance of meteoric investigations in establishing the nature and origin of matter in the solar system has long been recognized. The extraterrestrial nature of the bodies that cause the meteor phenomenon in our atmosphere was first recognized in the years following the great Leonid shower of 1833. Most authorities currently agree that there. is no evidence for any meteoric matter with an immediate origin beyond the gravitational field of the sun [e.g., Whipple, 1967;Lovell, 1954]. There is still notable dissent on even this point, some investigators claiming that more precise measurements would show a small percentage of particles whose orbits are hyperbolic with respect, to the sun 1964]. By showing that the meteoroids associated with a number of showers moved in the same orbit as certain comets, the relationship between comets and meteoroids was established beyond any reasonable doubt. It is now commonly held that most• meteorolds (the term used to denote meteoric particles before terrestrial encounter) are sloughed off comets as a result of solar warming. The relationship between meteorolds and asteroids remains. less certain. Ast•eroids, or the minor planets, are the bodies that orbit, the sun, primarily in the space between the orbits of Mars and Jupiter. From the earth, we can detect only those with radii larger than about i kin, but collisions should have produced smaller bodies down to particulate sizes [Dohnanyi, 1969a]. A meteoroid whose maximum orbital distance from the sun (aphelion) is inside t•he asteroid belts is usually thought to be of asteroidal origin, although it is recognized that there are 239