T he Dallol protovolcanic area on the Danakil Depres s ion (Afar region, E thiopia) exhibits unique hydrothermal manifes tations in hypers aline context, yielding varied polyextreme phys icochemical conditions . P revious s tudies identified a wide archaeal divers ity in les s extreme brines but failed to identify microorganis ms thriving in either high-chaotropicity, low-wateractivity brines or hyperacidic-hypers aline Na-F e-rich brines . R ecently, we acces s ed s everal s mall lakes under intens e degas s ing activity adjacent to the R ound Mountain, wes t to the Dallol dome (Wes tern C anyon Lakes ; WC L1-5). T hey exhibited intermediate parameter combinations (pH~5, 34-41% NaC l-dominated s alts with relatively high levels of chaotropic Mg-C a s alts ) that s hould allow to better cons train life limits . T hes e lakes were overwhelmingly dominated by Archaea, encompas s ing up to 99% of prokaryotic 16S rR NA gene amplicon s equences in metabarcoding s tudies . T he majority belonged to Halobacteriota and Nanohaloarchaeota, the latter repres enting up to half of prokaryotic s equences . Optical and epifluores cence micros copy s howed active cells in natural s amples and divers e morphotypes in enrichment cultures . S canning electron micros copy coupled with energy-dis pers ive x-ray s pectros copy revealed tiny cells (200-300 nm diameter) epibiotically as s ociated with s omewhat larger cells (0.6-1 µm) but als o the pres ence of s ilica-dominated precipitates of s imilar s ize and s hape, highlighting the difficulty of dis tinguis hing microbes from mineral biomorphs in this kind of low-biomas s s ys tems .