Ancient beach ridges reveal climate secrets of Argentina's Inner Río de la Plata Estuary.
The Inner Río de la Plata Estuary in Argentina has been filling up with sediment over time. The sediment comes from rivers and creeks, and the area has been shaped by changes in sea level and climate patterns like ENSO. The researchers found that beach ridges formed every 13-14 years after a period of high flooding, and the estuary has been filling in with sediment for thousands of years. The current delta in the estuary is still growing at a rate of about 56-64 meters per year.