Lowering the center of gravity increase stability. Increasing stability is characterized by a large base support, a centralized center of gravity projection within the base support, a large body mass and high friction at the ground interface.
ocean floor
ocean surface
thermocline
Deep ocean currents primarily flow along the ocean floor, driven by variations in water density. The halocline and thermocline are transitional layers in the ocean, but do not direct deep current flow.
Deep currents in the ocean predominantly flow along the ocean floor. These are also known as deep-ocean or abyssal currents. Unlike surface currents, which are mainly driven by wind, deep ocean currents are driven by variations in water density, which involves factors such as differences in temperature and salinity. The halocline and thermocline refer to transitional layers within the ocean where salinity and temperature change rapidly, respectively. However, they do not necessarily direct the flow of deep currents.
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