The Scientists have found signs of some of the earliest known earthquakes in 3.3-billion-year-old rocks.
The rocks provide early evidence of plate tectonics, which explains Earth's crust as split into large plates that glide across the mantle.
The rocks also point to what conditions may have been like when life first evolved.
This discovery has made while investigating the Barberton Greenstone Belt, a complex geological formation in southern Africa.
The belt is remarkably similar to much younger rocks in New Zealand.
They have experienced earthquake-triggered submarine landslides along the Hikurangi subduction zone.
The Barberton Greenstone, named after its greenish hue, provides one of the most extensive geological records for Earth between 3.2 billion and 3.6 billion years ago.