Tsunami-related deposits occur in Upper Miocene (uppermost Tortonian–lowermost Messinian) temperate carbonates in the Sorbas Basin, SE Spain. These carbonates exhibit two distinct depositional models. At the northern margin, small, locally steepened ramps developed on an irregular palaeotopography. These ramps displayed bryozoan accumulations at the toe of submarine cliffs changing laterally to coralline algal rudstones to floatstones. A gentle homoclinal ramp extended along the southern margin of the basin. Bivalve (brachiopod/bryozoan)-rich carbonates formed in the mid-ramp, whereas coralline algal-rudstones spread over the outer-ramp, changing basinwards to packstones with planktonic foraminifers. During the tsunami event large amounts of sediment were eroded from the carbonate ramps and redeposited. Two types of tsunami deposits are intercalated in outer-ramp sediments at both margins of the basin. In the steep outer-ramps of the northern margin, some folded layers are eroded and overlain by convex upward, stratified megahummocks. In the southern ramp, an abnormal thick shell-debris bed (TSB) occurs. Distinctive sedimentary features of these tsunamites and the inferred inflow and backflow effects were controlled by different palaeotopographic profiles. At the northern margin, inflow tsunami wave(s) struck the steep ramps, causing folding of underlying beds and excavating a large, irregular erosive surface. Backflow surges filled the inflow scours with the removed sediment, producing the megahummocky sets. At the southern margin, incoming tsunami surge(s) crossed the gentle ramp and eroded the sediments, especially in the inner-ramp settings. Backwash transported part of the previously removed sediments basinwards, depositing them as a thick bioclastic bed on the outer-ramp. The triggering mechanism of the tsunamis was probably related to seismic events recorded in the adjacent Tabernas Basin as several coeval seismites.