Sand Waves and the Golden Gate
Seafloor mapping of the San Francisco Bay and surrounding areas by marine scientists at the U.S. Geological Survey Pacific Coastal & Marine Science Center and Cal State University at Monterey Bay's Sea Floor Mapping Lab (SFML) is important for keeping shipping lanes safe, understanding pollution dispersal, mapping habitats, and much more.
Mapping of the underwater topography (called bathymetry) reveals landscapes fundamental to understanding the Bay Area's unique geology. The Golden Gate strait connects the San Francisco Bay to the open Pacific Ocean and is only one mile across.
Although the tidal range in the Bay Area is not incredibly large, the narrowness of the Golden Gate creates a funneling effect:
"Large volumes of water move into and out of San Francisco Bay as the tidal level of the Pacific Ocean just outside the Golden Gate changes each day. When the tide is changing from low to high levels, a flooding current moves water inland from (and through) the Golden Gate. When the tide is changing from high to low levels, an ebbing current moves water from inside the Bay toward (and through) the Golden Gate."
The image above (from Cal State Monterey Bay) is a perspective image looking towards the east. The colors represent water depth with the reds and yellows as shallower water and the blue and purple deeper water. The prominent patterns in the foreground might look like ripple marks on the beach, but these sand waves are similar in scale to some sand dunes seen in deserts — up to 30 feet tall and more than 700 feet from crest to crest.
The vigorous currents funneled through the Golden Gate continuously move sediment from underneath the bridge where it accumulates as these sand waves. But remember, this is a static snapshot of very dynamic systems. I'd love to see multiple repeat surveys that show how the field of sand waves change over time.