We show that the iron K emission line from MCG-6-30-15 could be broade
ned through Comptonization by a surrounding highly ionized cloud with
radius similar to 10(14) cm. We calculate the temperature of the cloud
to be similar to 0.21 keV, provided that a reasonable estimate of the
UV flux is made. The X-ray/gamma-ray emission observed from the sourc
e is compatible with this model. Such a cloud should be highly ionized
, and strong absorption edges are not expected from the source. For a
10(6) M-circle dot black hole the size of the cloud corresponds to abo
ut 300 Schwarzschild radii. The intrinsic line could then be emitted f
ar from the black hole, and gravitational redshift and Doppler effects
would be negligible. If the black hole mass is much larger than 10(6)
M-circle dot, gravitational/Doppler redshifts would also contribute s
ignificantly to the broadening. We argue that the broad red wing obser
ved in the source does not by itself imply emission from regions close
(R < 5r(S)) to the black hole. However, Comptonization cannot produce
a double peak. The presence of such a feature is a clear sign of inne
r disk emission influenced by gravitational and Doppler effects, perha
ps broadened by the Comptonization. We note that simultaneous broadban
d (2-100 keV) study of this source can also reveal (or rule out) the p
resence of such a Comptonizing cloud.