The coastal transition zone is an underexplored frontier in hydrology and geoscience

We have better maps of the surfaces of Venus, Mars, and the Moon than of the Earth's seafloor. There is even less information available about the geologic structure below the seafloor. In particular, the transition zone deep beneath and crossing the coastline is a very poorly studied frontier resulting from limitations of technology and logistical barriers. Here, we point out the significance of this region for understanding fundamental geologic processes, geohazards, and especially coastal aquifers. One prominent example is the increasing awareness of the importance of groundwater exchange between land and sea. This Perspective defines the region beneath the coastal transition zone, or coastal white ribbon as an underexplored frontier, and highlights the need for characterization of this critical region to depths of tens of km. We discuss available geophysical methods and their limitations with coastal groundwater used as the primary illustration. Advances in geophysical and drilling technology, coupled with numerical modeling, are needed to enable better accounting of this poorly understood component of the geosphere.

Automated summary

This article highlights the lack of research on marine geological structures, especially regarding the topography and geology below the coastline. Studying this area is significant for understanding geological processes, hazards, and coastal aquifers.