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.

143 point of view, was located in the middle longitudinal section of the aft part of the Atlantis II seamount model. The results of visual researches, which were recorded above the water surface in the x-y plane (Fig. 4b), showed that colored dyes wrap around the surface of the seamount from its lateral sides. At the same time, red and black dyes wrap around the mountain from one side and black ink moved at a greater distance than red. With distance from the mountain surface in the oscillatory motion of colored dye jets, intense modulating low-frequency oscillations occurred and large-scale jet clouds of a mixture of red and black dyes at a distance of about x=2H gradually moved to the median longitudinal section of the trace of the Atlantis II seamount model. Green dye jets, oscillating, expanding and wrapping around the lateral surface of the seamount from the side of the gorge of the Atlantis II seamount of volcanic origin, gradually degenerated in the near trace of the mountain model, as shown in Fig. 4b. The next depth of the color dye supply system was 0.5H from the top of the rough model of the Atlantis II seamount, the results of visual researches of which are presented in Fig. 5. The red dye was supplied along the center of the mountain ridge y=0 at a level of 0.10 m below the mountain top, or z=-0.5H and at a distance of 1 cm from the mountain, x=-0.05H, the green dye was supplied at the edge of the mountain ridge at a distance of 0.055 m from the center of the mountain closer to the gorge between the mountains (edge of the ridge y=0.28H), the black dye was supplied from the opposite edge of the mountain at a distance z=-0.28H.