Photo J.Thomson@GNS Science
The rocks at Kiritehere are part of what geologists call the Murihiku Supergroup (deposited 260 to145 million years ago). These rocks extend from port Waikato all the way down and round to the southeast coast of the South Island. They were laid down in a vast depression that had a chain of volcanoes alongside it. A lot of the sediments contain volcanic ash washed into them. The shellbed containing the fossils is called the Arawi formation which is only one of many formations in the Murihiku Supergroup. The fossils are dominated by scallop-like clams that belong to an extinct genus called monotis, but there are also other types too, such as brachiopods (lamp shells), occasional ammonites, or extremely rare marine reptile bones.