If you look at a zero-mean MA process:
$X_t = \varepsilon_t + \theta_1 \varepsilon_{t-1} + \cdots + \theta_q \varepsilon_{t-q} \,$
then you could regard the right hand side as akin to a weighted moving average of the $\varepsilon$ terms, but where the weights don't sum to 1.
For example, Hyndman and Athanasopoulos (2013) [1] say:
Notice that each value of $y_t$ can be thought of as a weighted moving average of the past few forecast errors.
Similar explanations of the term may be found in numerous other places. (In spite of the popularity of this explanation, I don't know for certain that this is the origin of the term, however; for example perhaps there was originally some connection between the model and moving-average smoothing.)
Note that Graeme Walsh points out in comments above that this may have originated with Slutsky (1927) "The Summation of Random Causes as a Source of Cyclical Processes"
[1] Hyndman, R.J. and Athanasopoulos, G. (2013) Forecasting: principles and practice. Section 8/4. http://otexts.com/fpp/8/4. Accessed on 22 Sept 2013.