Measurements of the electron temperature, T e , and density, n e , during the energy quench of a major disruption showed that the onset of T e erosion in the neighborhood of the m/nϭ2/1 O point at the low field side ͑LFS͒ accelerates the well-known m/nϭ1/1 erosion of the core temperature. During this phase T e (r) is only partially flat in the region between the qϭ2 and the qϭ1 surfaces and n e (r) decreases in the core and increases inside the m/nϭ2/1 island. Immediately after the flattening of T e (r) a large peak in T e and to a lesser extent in n e has been observed. This peak is radially localized at the qϭ2 radius at the LFS, is very short lived and is poloidally asymmetric. T e profiles measured by the heterodyne radiometer and the Thomson scattering agree very well up to the time T e (r) flattens but afterwards can be a factor of two different.