Toutatis was first sighted on 10 February 1934, and was named 1934 CT, but was lost soon afterwards. The spectral properties suggest that this is an
S-type, or stony asteroid, consisting primarily of
silicates. It has a moderate
Bond albedo of 0.13.
Radar imagery shows that Toutatis is a highly irregular body consisting of two distinct lobes, with maximum widths of about 4.6 km and 2.4 km, respectively. It is hypothesized that Toutatis formed from two originally separate bodies which coalesced at some point (a
contact binary), with the resultant asteroid being compared to a
rubble pile. Its rotation combines two separate periodic motions into a non-periodic result; to someone on the surface of Toutatis, the
Sun would seem to rise and set in apparently random locations and at random times at the asteroid's horizon. It has a
rotation period around its long axis (Pψ) of 5.38 days. This long axis is
precessing with a period (Pφ) of 7.38 days. The asteroid may have lost most of its original angular momentum and entered into this tumbling motion as a result of the
YORP effect. == Orbit ==