Rocks can
tell us a lot about the history of an area by their composition, shape, texture
and arrangement. In this installment of Reading Rocks, we will learn how to read
the tectonic history written in rocks.
Pushing,
pulling and sliding
Earth’s
tectonic plates move at about the same speed as your fingernails grow. We don’t
usually notice this movement, but over millions of years the continents are
rearranged, mountains and valleys form, oceans appear and disappear. The story
of these huge changes can be seen in rocks.
When rocks are
pushed or pulled by tectonic forces they bend, stretch and break. The breaks
are called faults. By looking at a fault, we can tell what forces caused the
break. This indicates the type of plate boundary or local forces that were
acting on the rock. Road cuttings and cliffs are good places to look for
faults.
This normal
fault was caused by pulling forces. (L Adikashvili 2016, Wikimedia Creative
Commons)
Reverse
faults and folds in this sandstone were caused by pushing forces. (J St John
2010, Wikimedia Creative Commons)
Video:
- Plate Tectonics(BrainPOP)
- Types of faults – simple and detailedexplanation(IRIS Earthquake Science)
Webpages:
- Types of tectonic boundaries (NOAA)
Landforms
at plate boundaries
You can spot
faults in a cross section of rock, but major landforms also tell us about
tectonic interactions. Jagged mountains are formed by continental collisions, whilst
rift valleys form as continents are pulled apart.
The
Himalayas, seen here from the International Space Station, were formed when the
Indian subcontinent collided with the Eurasian plate. (NASA 2004, Public
domain)
East
African Rift, seen from the International Space Station, is being formed as the
African and Somalian plates move away from each other. (NASA 2012, Public
domain)
Modelling
plate boundaries at home
How can we
model tectonic forces and see their effects? You can try this at home in
several ways.
Model forces using a Mars Bar and eat your work afterwards.
Build a
model using a plastic container, sand, soil and cardboard. Watch the video to learn
how to build this model.