"We are looking at the data currently, but we are expecting to see deformation over whole of New Zealand, from millimetres to metres," she said.
"As soon as we get the new data in, we'll re-measure our sites."
Because of the complex nature of what was happening to the Earth's crust, the observed displacement didn't move in any one direction.
Previous surveys had shown the country was moving by 4cm a year but, rather than shifting as a whole, tectonic forces were deforming the land surface - stretching, slimming and sliding it southward.
While the Bay of Plenty had been stretching apart by around 4cm each year, Wellington was being squeezed together by a similar amount.
Different regions were moving at different rates and in different directions - in some places this movement was increasing the stress in the earth's crust, while in other places it is releasing stress.
Scientists had been able to use the GPS data to simulate the country's distortion over a four-million-year period without allowing for earthquake impacts.
It projected much of the South Island and the lower North Island slimming into a skinnier tract of land, while the North Island rotates around and both islands grow closer together.