The mass of extraterrestrial material accreted by the Earth as submill
imeter particles has not previously been measured with a single direct
and precise technique that samples the particle sizes representing mo
st of that mass. The flux of meteoroids in the mass range 10(-9) to 10
(-4) grams has now been determined from an examination of hyper-veloci
ty impact craters on the space-facing end of the Long Duration Exposur
e Facility satellite. The meteoroid mass distribution peaks near 1.5 x
10(-5) grams (200 micrometers in diameter), and the small particle ma
ss accretion rate is (40 +/- 20) x 10(6) kilograms per year, higher th
an previous estimates but in good agreement with total terrestrial mas
s accretion rates found by geochemical methods. This mass input is com
parable with or greater than the average contribution from extraterres
trial bodies in the 1-centimeter to 10-kilometer size range.