<![CDATA[This study aims to reconstruct the tsunami event on December 22, 2018, due to the eruption of Mount Anak Krakatau which caused flank collapse generated an underwater landslide. Then this landslide caused a tsunami that impacted along the coast of the Sunda Strait, especially on the coast of Pandeglang Regency. Based on satellite imagery, it is known that the source of the landslide came from the southwestern part of Anak Krakatau's wall moving down the former caldera wall of the 1883 Krakatau volcanic eruption. The mount grew again and was known as Mount Anak Krakatau and appeared above sea level in 1929 and continued to grow. Subsequently, several eruptions spewed sediment deposits that had accumulated on the edges and foot of the mount. These sediments increased and become unstable, causing flank collapse and triggering underwater landslides. Several simulation scenarios have been carried out, in order to obtain the best model that can represent the 2018 Anak Krakatoa Tsunami with landslide parameters, namely: the volume of the landslide is 0.276 km3, the duration of propagation is 410 seconds, the inclination angle is 8.2°, and the length of the landslide trajectory is 3435 meters. The waveform generated as a tsunami source is in the form of wave peaks in the direction of the slide and wave valleys on the back of the slide. Furthermore, this wave propagated to all directions however mostly focused towards the southwest i.e. Panaitan Island and Pandeglang Regency. Tsunami simulations show that the tsunami reached: Panaitan Island and Pandeglang Regency at 58-60 minutes, Kota Agung (Lampung) at 42 minutes, and Ciwandan (Banten) at 46 minutes after the landslide with a tsunami height of 5.01m, 0.9 m and 0.7 m respectively, with a maximum tsunami wave height of 18.6 m on Panaitan Island. Furthermore, it is known that there are 5 areas in Pandeglang Regency that fall into the high tsunami hazard category with a tsunami height of more than 3 m, namely Panaitan Island, Ujungkulon District, Sumur, Panimbang, and Labuhan. By knowing the distribution tsunami height and estimate time arrival of the tsunami in the affected area, as well as the inundation area accurately, an early warning system and mitigation efforts can be planned such as spatial planning and other efforts]]>
