The densest place of ocean isobath is.

Best answer: Continental slope. Isobathic line refers to the closed curve formed by connecting points with the same depth in the ocean or lake, which is vertically projected onto the plane after being scaled down. The curve formed is called isobath. The depth of each point on the same isobath is equal. Seawater depth refers to the vertical distance between the depth datum and the seabed, and the average low tide level is usually used as the depth datum. Mainly used to show the depth and topography of the ocean.

The densest place of marine isobathymetry is the continental slope. Isobathic line refers to the closed curve formed by connecting points with the same depth in the ocean or lake, which is vertically projected onto the plane after being scaled down. The curve formed is called isobath. The depth of each point on the same isobath is equal. Seawater depth refers to the vertical distance between the depth datum and the seabed, and the average low tide level is usually used as the depth datum. Mainly used to show the depth and topography of the ocean. There are three types of isobaths on charts: basic isobaths, supplementary isobaths and imprecise isobaths.