The M_w 6.9 Samos earthquake occurred on 30 October 2020 11:51 offshore of the Samos island, west of the Kuşadası bay in the Aegean Sea. The earthquake caused destruction in villages of Greece and Turkey. The earthquake intensity reached a maximum of VII in İzmir–Bayraklı. A tsunami followed the shock and hit many villages around Samos and the Kuşadası bay. The Sığacık village of Izmir-Turkey suffered heavily from the tsunami. A post-event field survey in Sığacık has been conducted on 31 October 2020, and measurements of flow depth, run-up and limits of inundation were collected. The tsunami inundated the entire coastal area in Sığacık for at least 200 m inland. The maximum inundation has been observed NE of Sığacık. Sea water reached a distance of 391 ± 2 m. The maximum run-up is measured as 5.3 ± 0.3 m north of Sığacık. This is the highest value for the Samos tsunami measured along the Greek and Turkish coastal areas. The high run-up value is attributed to the elongated geometry of the Sığacık bay, the shallow seafloor, the low and flat land morphology in Sığacık and to the existence of four > 70-m-long E–W trending channels. The tsunami left limited amount of clay to sand size sediments forming a layer of less than 2–3 cm in the depression areas in Sığacık. The limited amount of evidence remained from the tsunami of this M_w 6.9 earthquake in Sığacık (a location with significant inundation and the highest run-up value) signifies the difficulty of palaeo-tsunami surveys for the Aegean Sea region.

在中号_{w ^}6.9萨摩斯岛地震发生在2020年10月30日11:51，位于爱琴海Kuşadası湾以西的萨摩斯岛海上。地震在希腊和土耳其的村庄造成破坏。在伊兹密尔—贝拉克利，地震烈度最高达到七级。地震发生后，海啸席卷了萨摩斯岛和库萨达斯海湾的许多村庄。伊兹密尔土耳其的Sığacık村庄遭受了海啸的沉重打击。到2020年10月31日，在Sığacık进行了事后现场调查，并收集了水流深度，径流和淹没极限的测量值。海啸淹没了Sığacık的整个沿海地区，至少内陆200 m。已经观察到最大的淹没发生在Sığacık。海水达到391±2 m的距离。在锡耶克（Sığacık）以北的最大径距为5.3±0.3 m。这是沿希腊和土耳其沿海地区测得的萨摩斯海啸的最高值。较高的上升值归因于Sığacık海湾的拉长的几何形状，浅海底，Sığacık的低低平坦的土地形态以及存在四个> 70米长的E–W趋势通道。海啸使少量的粘土留给沙粒大小的沉积物，在锡克阿奇克（Sığacık）的洼地地区形成了一个少于2–3 cm的层。这次海啸仍然留下了有限的证据 海啸使少量的粘土留给沙粒大小的沉积物，在锡克阿奇克（Sığacık）的洼地地区形成了一个少于2–3 cm的层。这次海啸仍然留下了有限的证据 海啸使少量的粘土留给沙粒大小的沉积物，在锡克阿奇克（Sığacık）的洼地地区形成了一个少于2–3 cm的层。这次海啸仍然留下了有限的证据中号_W¯¯在Sığacık6.9级地震（有显著淹没，最高助跑值的位置）表示为爱琴海地区古海啸调查的难度。