It was possible they may float to the surface of their own accord and wash up anywhere along New Zealand's east coast.
They were marked with the contact information of either GNS Science, or Columbia University on the side of them.
"The information recorded on the instruments is very valuable to us, and we would love to hear from anyone if they find one of these sensors washed up on the shore," Wallace said.
Initial data from those instruments that had been collected suggested many more earthquakes were happening off the North Island's East Coast than could be detected by the onshore network of instruments operated by GeoNet.
The data collected helps scientists learn more about earthquakes and so-called "slow slip" events at the subduction zone, and what this meant for future earthquakes in New Zealand.
Wallace said the focus of the research project will help to understand how, why, and how often the Hikurangi subduction zone moved in slow-slip events and large earthquakes.
Although there have been cases of slow slip events preceding big quakes – like Tohoku in Japan in 2011 – such instances were rare, so scientists say they shouldn't be seen as warning signals.
This research was being undertaken under a five-year MBIE-funded Endeavour project led by GNS Science, with major collaboration and contributions from other New Zealand and international partners.
Anyone who found one of the instruments should phone GNS Science at 04 570 1444.