
How can there be ripple marks on the seabed at a depth of 4000 meters?
This paper answers the question of why there are ripples on the 4000-meter deep seabed, introduces the definition and geological significance of ripples, and explains that shallow sea ripples are formed by sea surface waves stirring up sediment. Through the HEBBLE Deep Sea Observation Program, scientists discovered that the flow along the isobath is the cause of deep sea ripples. At the same time, the program also observed the phenomenon of deep sea storms. The discovery of deep sea currents has changed people's understanding of the deep sea environment.
