Activity

Rock layers and relative dating

Most sedimentary rocks are laid down in flat, horizontal layers. These can later tilt and fold due to tectonic activity, and river cuttings can cause gaps among the layers. Geologists are able to ‘read’ the rock layers using relative and absolute dating techniques. Relative dating arranges geological events – and the rocks they leave behind – in a sequence. The method of reading the order is called stratigraphy (layers of rock are called strata).

In this activity, students observe rock layers located near Whanganui, watch an animation about how they were formed and use relative dating to work out the order in which rocks were created. The activity offers literacy opportunities as well as practice using the science capability ‘Interpret representations’.

thinnest rock
second oldest rock
oldest rock pre-tilt
youngest rock post-tilt
oldest rock post-tilt
youngest rock pre-tilt

Relative rock layers

Use this interactive to work out the relative ages of some rock layers from youngest to oldest. Drag and drop the text labels onto the diagram.

Go here to find out more about how to use this interactive.

Rights: The University of Waikato Te Whare Wānanga o Waikato

By the end of this activity, students should be able to:

  • observe, discuss and compare rock layers in a photo and a diagram

  • use reading skills to correctly label an interactive rock layer diagram

  • use oral and written language skills to narrate a video animation about rock layer formations.

Download the Word file (see link below) for:

  • background information for teachers

  • teacher instructions

  • student instructions.

Nature of science

Scientists use diagrams and models to communicate information. Students need support and practice to become familiar with and know how to use these science communication tools.

Related content

This activity is part of our collection on dating the past. The introductory article has links to related articles, activities and media.

Published: 14 March 2018