"The storm obviously generated huge amounts of sediment and threw up large amounts of coral on to the islands, which has helped them to re-organise themselves."
In effect, new islands had been formed on the sites of previous ones.
"They change, they move, they shift - you'll have a period of erosion on one part and a period of accretion on the other."
Dr Ford, who lived in the Marshall Islands for three years, said the changes were rapid and indicate that reef island formation can occur quickly.
"Evidence suggests that despite the typhoon occurring over a century ago the geomorphic adjustment of islands is still on-going," he said.
"The take-home message is really that a high magnitude event can both destroy the islands, and set about a series of processes that enables them to return."
By better understanding the complicated and dynamic nature of island formation, scientists would better under stand their response to sea level rise as the globe warmed, he said.
The study is part of wider work by the university investigating the geomorphology of Pacific islands.