13The Mojave Desert presents an array of Pleistocene lacustrine deposits and aeolian landforms to 14 which, at times, it has proved challenging to apply luminescence methods. We tested the suitability 15 of K-feldspar post-IR IRSL methods using two sites with independent radiocarbon dating -shorelines 16 at Harper Lake and Silver Lake -considering: 1) overall performance of the post-IR IRSL 225°C 17 (pIRIR225) protocol, 2) effect of test dose size on pIRIR225 De, 3) anomalous fading correction of 18 pIRIR225 ages; 4) preliminary single grain pIRIR225 results. 19We observe consistently good performance of the single aliquot pIRIR225 protocol, with good dose 20 recovery, acceptable recycling ratios, low recuperation and low inter-aliquot scatter. The pIRIR225 21 ages for Silver Lake (8.8 ± 0.4 and 11.3 ± 0.5 ka) and Harper Lake (both 25.4 ± 1.4 ka) are in 22 substantially better agreement with the independent dating than low temperature (50°C) IRSL and 23 quartz OSL ages. pIRIR225 fading rates are reduced to ~2.0-2.5% per decade, but there remains a 24 tendency for under-estimation when using uncorrected ages. A need for fading correction is further 25 implied at Harper Lake via comparison with multi-elevated temperature (MET)-PIR age plateaus and 26 pIRIR290 measurements, although at the younger Silver lake site these methods produce ages nearly 27 identical to the uncorrected pIRIR225 ages.