We present B, V, and R band photometry for three of the six known Cent
aur objects. We have measured V-R colors of 0.47+/-0.04 and 0.77+/-0.0
5 for the Centaurs 1995 GO and 1993 HA(2), respectively, as well as a
B-V color of 0.75+/-0.04 for 1995 GO. We have measured B-V and V-R col
ors for the Centaur 5145 Pholus that closely agree with previous measu
rements in the literature. We have found that the four Centaurs with k
nown colors can be separated into two groups, one group with near sola
r colors (2060 Chiron and 1995 GO) and the other with very red colors
(5145 Pholus and 1993 HA(2)). Centaurs with solar colors may have surf
aces rich in icy, primitive, carbonaceous chondrite like material whil
e Centaurs that have very red surfaces may have icy surfaces rich in c
omplex carbon bearing molecules. The differences in the surfaces of Ce
ntaurs may result from differences in their primordial composition. Pe
rhaps, 5145 Pholus and 1993 HA, had higher initial concentrations of s
imple ice components (e.g., CH4) than 2060 Chiron and 1995 GO that upo
n cosmic ray or solar wind bombardment produced larger amounts of red
colored complex organic molecules. Alternatively, Centaurs may have or
iginated with similar initial compositions and thermal processing and
coma formation may have altered the surface composition and hence the
color of Centaurs closer to the Sun, 1995 GO (perihelion distance, q=6
.85 AU) and 2060 Chiron (q=8.45 AU), but not the composition and hence
the red color of Centaurs farther from the Sun, 5145 Pholus (q=8.68 A
U) and 1993 HA(2) (q=11.83 AU). (C) 1997 American Astronomical Society
.