Proceedings of the International scientific and practical conference ―Education and Scientific Progress‖ (April 24-26, 2026) / Publisher website: www.naukainfo.com. – Manchester, United Kingdom, 2026. - 218 p.

141 model, the jets of colored dyes begin to rise to the top of the mountain, and then the jets of black and green dyes oscillate around the top of the mountain, each on its own side (Fig. 3b). The jet of red dye in front of the top of the mountain expanded and began to form a vortex structure elongated in the transverse direction, the core of which had a scale along the coordinate x=(0.05-0.1)H, and along the coordinate y=(0.15-0.25)H. At a distance of about the length of the seamount crest, a larger and less intense vortex structure with a scale of almost x=H and y=0.75H was observed. Black and green dyes were also observed on different sides of this vortex structure. Then all these colored dyes merged into a large-scale multi-colored cloud that exceeded the length of the ridge of the Atlantis II seamount model. The green dye, wrapping around the top of the seamount model, expanded significantly and, under the influence of the flow in the gorge between the seamount models, headed towards the midsection of Atlantis II and merged with the vortex structures that carried the jets of red dye. а b Fig. 4. Visualization of the Atlantis II seamount model for the coordinates of the red dye supply (x=-0.05H; y=0; z=-0.35H):the side (a) and the top (b) The results of visualization with subsequent deepening of colored dyes to a depth of -0.35H are presented in Fig. 4. Here, the red dye was supplied along the center of the mountain ridge y=0 at a level of 0.07 m below the mountain top, or y=- 0.35Н and at a distance of 1 cm from the mountain, x=-0.05Н, the green dye was supplied at the edge of the mountain ridge at a distance of 0.055 m from the center of